Applied Mathematical Sciences I Volume 1 Fritz John Partial Differential Equations Third Edition Springer-Verlag New York· Heidelberg· Berlin Fritz John Courant Institute of Mathematical Sciences New York University New York, NY 10012 USA Editors Fritz John Lawrence Sirovich Courant Institute of Mathematical Sciences New York University New York, NY 10012 USA Division of Applied Mathematics Brown University Providence, RI 02912 USA Joseph P. LaSalle Gerald B. Whitham Division of Applied Mathematics Brown University Providence, RI 02912 USA Applied Mathematics Firestone Laboratory California Institute of Technology Pasadena, CA 91125 USA AMS Subject Classifications: 35-02, 35AIO, 35EXX, 35L05, 35LlO Library of Congress Cataloging in Publication Data John, Fritz 1910Partial differential equations. (Applied mathematical sciences; v. I) Bibliography: p. Includes index. I. Differential equations, Partial. I. Title. II. Series. QAl.A647 vol. I 1978 [QA374] 510'.8s [515'.353] 78-10449 All rights reserved. No part of this book may be translated or reproduced in any form without written permission from Springer-Verlag. Copyright © 1971, 1975, 1978 by Springer-Verlag New York Inc. Softcover reprint ofthe hardcover 3rd edition 1978 ISBN -13: 978-1-4684-0061-8 DOl: 10.1007/978-1-4684-0059-5 e-ISBN -13: 978-1-4684-0059-5 Preface to the Third Edition The book has been completely rewritten for this new edition. While most of the material found in the earlier editions has been retained, though in changed form, there are considerable additions, in which extensive use is made of Fourier transform techniques, Hilbert space, and finite difference methods. A condensed version of the present work was presented in a series of lectures as part of the Tata Institute of Fundamental Research -Indian Institute of Science Mathematics Programme in Bangalore in 1977. I am indebted to Professor K. G. Ramanathan for the opportunity to participate in this exciting educational venture, and to Professor K. Balagangadharan for his ever ready help and advice and many stimulating discussions. Very special thanks are due to N. Sivaramakrishnan and R. Mythili, who ably and cheerfully prepared notes of my lectures which I was able to use as the nucleus of the present edition. A word about the choice of material. The constraints imposed by a partial differential equation on its solutions (like those imposed by the environment on a living organism) have an infinite variety of consequences, local and global, identities and inequalities. Theories of such equations usually attempt to analyse the structure of individual solutions and of the whole manifold of solutions by testing the compatibility of the differential equation with various types of additional constraints. The problems arising in this way have challenged the ingenuity of mathematicians for centuries. It is good to keep in mind that there is no single "central" problem; new applications ·commonly lead to new questions never envisioned before. In this book emphasis is put on discovering significant features of a differential equation, and on exploring them as far as possible with a limited amount of machinery from mathematical analysis. Entanglement in a mass of technical details has been avoided, even when this resulted in less general or less complete results. New Rochelle, N. Y. Fritz John v Contents Chapter 1 The single first-order equation 1 I. Introduction 2. Examples 3. Analytic Solution and Approximation Methods in a Simple Example Problems 4. Quasi-linear Equations 5. The Cauchy Problem for the Quasi-linear Equation 6. Examples Problems 7. The General First-order Equation for a Function of Two Variables 8. The Cauchy Problem 9. Solutions Generated as Envelopes Problems I 2 4 8 8 10 14 18 19 23 28 30 Chapter 2 Second-order equations: hyperbolic equations for functions of two independent variables l. Characteristics for Linear and Quasi-linear Second-order Equations 2. Propagation of Singularities 3. The Linear Second-order Equation Problems 4. The One-Dimensional Wave Equation Problems 31 31 33 35 37 38 43 vii Contents 5. 6. Systems of First-order Equations (Courant-Lax Theory) A Quasi-linear System and Simple Waves Problem 44 50 51 Chapter 3 Characteristic manifolds and the Cauchy problem 52 1. Notation of Laurent Schwartz Problems 2. The Cauchy Problem Problems 3. Cauchy-Kowalewski Theorem Problems 4. The Lagrange-Green Identity 5. The Uniqueness Theorem of Holmgren 6. Distribution Solutions Problems 52 53 54 59 59 63 64 65 67 70 Chapter 4 The Laplace equation 1. Green's Identity, Fundamental Solutions Problems 2. The Maximum Principle Problems 3. The Dirichlet Problem, Green's Function, and Poisson's Formula Problems 4. Proof of Existence of Solutions for the Dirichlet Problem Using Subharmonic Functions ("Perron's Method") Problem 5. Solution of the Dirichlet Problem by Hilbert-Space Methods Problems 72 72 79 81 83 84 88 89 94 94 101 Chapter 5 Hyperbolic equations in higher dimensions 1. V1ll The Wave Equation in n-dimensional Space (a) The method of spherical means Problems (b) Hadamard's method of descent Problems (c) Duhamel's principle and the general Cauchy problem Problem (d) Initial-boundary-value problems ("Mixed" problems) Problems I 103 103 103 109 110 III 112 116 116 119 Contents 2. Higher-order Hyperbolic Equations with Constant Coefficients (a) Standard form of the initial-value problem Problem (b) Solution by Fourier transformation Problems (c) Solution of a mixed problem by Fourier transformation (d) The method of plane waves Problems 3. Symmetric Hyperbolic Systems (a) The basic energy inequality Problems (b) Existence of solutions by the method of finite differences Problems 120 120 122 122 132 133 135 138 139 139 145 146 155 Chapter 6 Higher-order elliptic equations with constant coefficients 1. The Fundamental Solution for Odd n Problems 2. The Dirichlet Problem Problems 156 157 159 160 164 Chapter 7 Parabolic equations 1. The Heat Equation (a) The initial-value problem Problems (b) Maximum principle, uniqueness, and regularity Problems (c) A mixed problem Problems 2. The Initial-value Problem for General Second-order Linear Parabolic Equations (a) The method of finite differences and the maximum principle (b) Existence of solutions of the initial-value problem Problems 166 166 166 173 174 179 179 181 181 181 185 188 Bibliography 191 Glossary 193 Index 195 ix The single first-order equation * 1 1. Introduction A partial differential equation (henceforth abbreviated as P.D.E.) for a function u(x,y, ... ) is a relation of the form F(x,y, ... ,u,ux,Uy, ... ,uxx,uxy, ... ) =0, (1.1) where F is a given function of the independent variables x,y, ... , and of the "unknown" function u and of a finite number of its partial derivatives. We call u a solution of (1.1) if after substitution of u(x,y, ... ) and its partial derivatives (1.1) is satisfied identically in x,y, ... in some region n in the space of these independent variables. Unless the contrary is stated we require that x,y, ... are real and that u and the derivatives of u occurring in (1.1) are continuous functions of x,y, ... in the real domain n.t Several P.D.E.s involving one or more unknown functions and their derivatives constitute a system. The order of a P.D.E. or of a system is the order of the highest derivative that occurs. A P.D.E. is said to be linear if it is linear in the unknown functions and their derivatives, with coefficients depending on the independent variables x,y, .... The P.D.E. of order m is called quasilinear if it is linear in the derivatives of order m with coefficients that depend on x,y, ... and the derivatives of order < m. • ([71, [131, [26D t For simplicity we shall often dispense with an explicit description of the domain n. Statements made then apply "locally," in a suitably restricted neighborhood of a point of X)' ••• -space. I The single first-order equation 2. Examples Partial differential equations occur throughout mathematics. In this section we give some examples. In many instances one of the independent variables is the time, usually denoted by t, while the others, denoted by X\,X2, ... ,Xn (or by x,y,z when n(;3) give position in an n-dimensional space. The space differentiations often occur in the particular combination a=£+ ... +£ axi ax; (2.1) known as the Laplace operator. This operator has the special property of being invariant under rigid motions or equivalently of not being affected by transitions to other cartesian coordinate systems. It occurs naturally in expressing physical laws that do not depend on a special position. (i) The Laplace equation in n dimensions for a function u(x\, ... ,xn) is the linear second-order equation (2.2) This is probably the most important individual P.D.E. with the widest range of applications. Solutions u are called potential functions or harmonic functions. For n=2, x\ =x, X2=Y' we can associate with a harmonic function u(x,y) a "conjugate" harmonic function v(x,y) such that the first-order system of Cauchy-Riemann equations ux = vy, Uy = - vx (2.3) is satisfied. A real solution (u,v) of (2.3) gives rise to the analytic function fez) = f(x+ ry) =u(x,y)+ iv(x,y) (2.4) of the complex argument z = x + ry. We can also interpret (u( x,y), - v(x,y» as the velocity field of an irrotational, incompressible flow. For n = 3 equation (2.2) is satisfied by the velocity potential of an irrotational incompressible flow, by gravitational and electrostatic fields (outside the attracting masses or charges), and by temperatures in thermal equilibrium. (ii) The wave equation in n dimensions for u=u(x\, ... ,xn,t) is (2.5) (c = const. > 0). It represents vibrations of strings or propagation of sound waves in tubes for n= 1, waves on the surface of shallow water for n=2, acoustic or light waves for n = 3. (iii) Maxwell's equation in vacuum for the electric vector E=(E\,E2,E3) and magnetic vector H=(H\,H2 ,H3) form a linear system of essentially 6 first-order equations eEt=curl H, pHt= -curl E (2.6a) divE=divH=O 2 (2.6b) 2 Examples with constants e, p.. (If relations (2.6b) hold for t = 0, they hold for all t as a consequence of relations (2.6a». Here each component E;,Hk satisfies the wave equation (2.5) with c 2 = 1/ ep.. (iv) Elastic waves are described classically by the linear system a a2u. P-i- = p.Llui +(A+ p.)-a (divu) Xi at (2.7) (i= 1,2,3), where the Ui (X 1,X2,x3,t) are the components of the displacement vector u, and p is the density and A, p. the Lame constants of the elastic material. Each Ui satisfies the fourth-order equation _A+2p. Ll)(l.:.. - .l!:Ll)U.=O, (l.:.. at2 at 2 p p (2.8) I formed from two different wave operators. For elastic equilibrium (ut=O) we obtain the biharmonic equation Ll2u = O. (2.9) (v) The equation of heat conduction ("heat equation") ut=kLlu (2.10) (k = const. > 0) is satisfied by the temperature of a body conducting heat, when the density and specific heat are constant. (vi) Schrodinger's wave equation (n=3) for a single particle of mass m moving in a field of potential energy V(x,y,z) is ilitf;t= - ;:Lltf;+ Vtf;, (2.11) where h = 2'1T1i is Planck's constant. The equations in the preceding examples were all linear. Nonlinear equations occur just as frequently, but are inherently more difficult, hence in practice they are often approximated by linear ones. Some examples of nonlinear equations follow. (vii) A minimal surface z = u(x,y) (i.e., a surface having least area for a given contour) satisfies the second-order quasi-linear equation (1 + uj)uxx -2ux uy uxy +(1 + u;)uyy =0. (2.12) (viii) The velocity potential q,(x,y) (for velocity components q,x,q,y) of a two-dimensional steady, adiabatic, irrotational, isentropic flow of density p satisfies (1- c- 2q,;)q,xx - 2c- 2q,Ayq,xy + (1- c- 2q,;)q,yy =0, (2.13) where c is a known function of the speed q=yq,;+q,; . For example y-1 c 2= 1- __ q2 2 for a polytropic gas with equation of state p=ApY. (2.14) (2.15) 3 I The single first-order equation (ix) The Navier-Stokes equations for the viscous flow of an incompressible liquid connect the velocity components Uk and the pressure p: au; -+ at L -au;u =---+y!:J.u., 1 ap k axk L k k aUk p ax.I I =0, aXk (2.l6a) (2. 16b) where p is the constant density and y the kinematic viscosity. (x) An example of Ii third-order nonlinear equation for a function u(x,t) is furnished by the Korteweg-de Vries equation (2.17) first encountered in the study of water waves. In general we shall try to describe the manifold of solutions of a P.D.E. The results differ widely for different classes of equations. Meaningful "well-posed" problems associated with a P.D.E. often are suggested by particular physical interpretations and applications. 3. Analytic Solution and Approximation Methods in a Simple Example* We illustrate some of the notions that will play an important role in what follows by considering one of the simplest of all equations ut+cux=O (3.1) for a function u= u(x,t), where c=const. >0. Along a line of the family (3.2) x- ct=const.=~ ("characteristic line" in the xt-plane) we have for a solution u of (3.1) du d dt = dtu(ct+~,t)=cux+Ut=O. Hence u is constant along such a line, and depends only on the parameter which distinguishes different lines. The general solution of (3.1) then has the form (3.3) u(x, t) =f(~) = f(x - ct). ~ Formula (3.3) represents the general solution u uniquely in terms of its initial values (3.4) u(x,O)= f(x). Conversely every u of the form (3.3) is a solution of (3.1) with initial values f providedf is of class C1(R). We notice that the value of u at any point (x,t) depends only on the initial valuefat the single argument ~=x-ct, the abscissa of the point of intersection of the characteristic line through *({16], [18], [2SD 4 3 Analytic Solution and Approximation Methods in a Simple Example -+-,~----------x Figure 1.1 (x, t) with the initial line, the x-axis. The domain of dependence of u(x, t) on the initial values is represented by the single point ~. The influence of the initial values at a particular point ~ on the solution u(x,t) is felt just in the points of the characteristic line (3.2). (Fig. 1.1) If for each fixed t the function u is represented by its graph in the ut-plane, we find that the graph at the time t = T is obtained by translating the graph at the time t = 0 parallel to the x-axis by the amount cT: u(x, 0) = u(x+ cT, T)= f(x). The graph of the solution represents a wave propagating to the right with velocity c without changing shape. (Fig. 1.2) We use this example with its explicit solution to bring out some of the notions connected with the numerical solution of a P.D.E by the method of finite differences. One covers the xt-plane by a rectangular grid with mesh size h in the x-direction and k in the t-direction. In other words one considers only points (x,t) for which x is a multiple of hand t a multiple of k. It would seem natural for purposes of numerical approximation to replace the P.D.E. (3.1) by the difference equation v(x,t+k)-v(x,t) v(x+h,t)-v(x,t) k +c h =0. (3.5) Formally this equation goes over into vt+cvx=O as h,k-+O. We ask to --~------~----------L----x x x + cT Figure 1.2 5 1 The single first-order equation what extent a solution v of (3.5) in the grid points with initial values v(x,O)= f(x) (3.6) approximates for small h,k the solution of the initial-value problem (3.1), (3.4). Setting A= k / h, we write (3.5) as a recursion formula v(x,t+ k)=(1 +AC)V(X,t) -ACV(X+ h,t) (3.7) expressing v at the time t+ k in terms of v at the time t. Introducing the shift operator E defined by (3.8) Ef(x) = f(x+ h), (3.7) becomes v(x,t+ k)=(1 +AC) -AcE)v(x,t) (3.8a) for t = nk this immediately leads by iteration to the solution of the initial-value problem for (3.5): v(x,t) = v(x,nk) =(1 +AC) -AcE Yv(x, 0) n = L (::Z)(1 +AC)m( -AcEy-mf(x) m=O L (::Z)(1 +AC)m( -Acr-mf(x+(n- m)h). n = (3.9) m=O Clearly the domain of dependence for v(x,t)=v(x,nk) consists of the set of points x, x+h, x+2h, ... , x+nh (3.10) on the x-axis, all of which lie between x and x + nh. The domain of the differential equation solution consists of the point ~ = x- ct = x - Mh, which lies completely outside the interval (x,x + nh). It is clear that v for h,k~O cannot be expected to converge to the correct solution u of the differential equation, since in forming v(x,t) we do not make use of any information on the value of f(~, which is vital for determining u(x, t), but only of more and more information onfin the interval (x,X+(t/A)) which is irrelevant. The difference scheme fails the Courant-Friedrichs-Lewy test, which requires that the limit of the domain of dependence for th~ difference equation contains the domain of dependence for the differential equation. That the scheme (3.5) is inappropriate also is indicated by its high degree of instability. In applied problems the data f are never known with perfect accuracy. Moreover, in numerical computations we cannot easily use the exact values but commit small round-off errors at every step. Now it is clear from (3.9) that errors in f of absolute value e with the proper (alternating) sign can lead to a resulting error in v(x,t)=v(x,nk) of size n e L (::Z)(1 +Ac)m(Acr-m=(1 +2ACre. m=O 6 (3.11 ) 3 Analytic Solution and Approximation Methods in a Simple Example Thus for a fixed mesh ratio A the possible resulting error in v grows exponentially with the number n of steps in the t-direction. A more appropriate difference scheme uses "backward" difference quotients: v(x,t+k)-v(x,t) v(x,t)-v(x-h,t) k +c h =0 (3.12) or symbolically vex, t+ k) = (I-AC) + AcE -1)V(X, t). (3.13) The solution of the initial-value problem for (3.13) becomes n v(x,t)=v(x,nk)= :L (::Z)(1-AC)m(Act-mf(x-(n-m)h). (3.14) m=O In this scheme the domain of dependence for points vex, t) on f consists of the x, x-h, x-2h, ... , x-nh=x- t X (3.15) Letting h, k~O in such a way that the mesh ratio A is held fixed, the set (3.15) has as its limit points the interval [x-(t/A),x] on the x-axis. The Courant-Friedrichs-Lewy test is satisfied, when this interval contains the point ~ = x - ct, that is when the mesh ratio A satisfies Ac": 1. (3.16) Stability of the scheme under the condition (3.16) is indicated by the fact that by (3.14) a maximum error of size e in the initial functionfresults in a maximum possible error in the value of v(x,t)=v(x,nk) of size n e :L (::Z)(1-AC)m(Act-m=e(I-AC)+Act=e. (3.17) m=O We can prove that the v represented by (3.14) actually converges to u(x,t)=f(x-ct) for h,k~O with k/h=A fixed, provided the stability criterion (3.16) holds andfhas uniformly bounded second derivatives. For that purpose we observe that u(x, t) satisfies lu(x,t+ k) -(I-Ac)u(x,t) -Acu(x- h,t)1 = If(x - ct- ck)- (I-Ac)f(x- ct)-Acf(x- ct- h)l..: Kh 2, (3.18) where (3.19) as is seen by expanding f about the point x - ct. Thus, setting w = u - v we have Iw(x,t+ k)-(1-Ac)w(x,t) -Acw(x- h,t)l..: Kh 2 7 1 The single first-order equation and hence sup Iw(x,t+ k)1 (;(I-Ac) sup Iw(x,t)1 +ACSUP IW(X- h,t)1 + Kh 2 x x x (3.20) = sup Iw(x,t)1 +Kh 2• x Applying (3.20) repeatedly it follows for t = nk that lu(x,t) - v(x,t)1 (; sup Iw(x,nk)1 x 2 Kth (;s~plw(x,O)I+nKh = T ' since w(x,O)=O. Consequently w(x,t)~O as h~O, that is, the solution v of the difference scheme (3.12) converges to the solution u of the differential equation. PROBLEMS 1. Show that the solution v of (3.12) with initial dataJ converges to u for h~O and a fixed A<; 1/ c, under the sole assumption that J is continuous. (Hint: the fact that both u and v change by at most e when we change J by at most e.) 2. To take into account possible round-off errors we assume that instead of (3.13) v satisfies an inequality Iv(x,t+ k)-(I-Ac)v(x,t)-Acv(x- h,t)1 <8. Show that for a prescribed 8 and for K given by (3.19) we have the estimate Kth t lu(x,t)- v(x,t)1 <; T + Ah 8 (3.21) assuming that (3.16) holds and that v(x, 0) =J(x). Find values for A and h based on this formula that will guarantee the smallest maximum error in computing u(x,t). 3. Instability of a difference scheme under small perturbations does not exclude the possibility that in special cases the scheme converges towards the correct function, if no errors are permitted in the data or the computation. In particular let J(x) = eax with a complex constant a. Show that for fixed x, t and any fixed positive A=k/h whatsoever both the expressions (3.9) and (3.14) converge for n ~ 00 towards the correct limit e a(x - CI). (This is consistent with the Courant-Friedrichs-Lewy test, since for an analytic J the values of J in any interval determine those at the point ~ uniquely.) 4. Quasi-linear Equations The general first-order equation for a function u=u(x,y, ... ,z) has the form f(x,y, ... ,u,ux'~'·· .,uz ) =0. (4.1) Equations of this type occur naturally in the calculus of variations, in particle mechanics, and in geometrical optics. The main result is the fact 8 4 Quasi-linear Equations that the general solution of an equation of type (4.1) can be obtained by solving systems of Ordinary Differential Equations (O.D.E.s for short). This is not true for higher-order equations or for systems of first-order equations. In what follows we shall mostly limit ourselves to the case of two independent variables x,y. The theory can be extended to more independent variables without any essential change. We first consider t~e somewhat simpler case of a quasi-linear equation a(x,y,u)ux + b(x,y,u)Uy = c(x,y,u). (4.2) We represent the function u(x,y) by a surface z = u(x,y) in xyz-space. Surfaces corresponding to solutions of a P.D.E. are called integral surfaces of the P.D.E. The prescribed functions a(x,y,z),b(x,y,z),c(x,y,z) define a field of vectors in xyz-space (or in a portion n of that space). Obviously only the direction of the vector, the characteristic direction, matters for the P.D.E. (4.2). Since (ux,Uy, -1) constitute direction numbers of the normal of the surface z = u(x,y), we see that (4.2) is just the condition that the normal of an integral surface at any point is perpendicular to the direction of the vector (a,b,c) corresponding to that point. Thus integral surfaces are surfaces that at each point are tangent to the characteristic direction. With the field of characteristic directions with direction numbers (a,b,c) we associate the family of characteristic curves which at each point are tangent to that direction field. Along a characteristic curve the relation ~ a(x,y,z) = • b(x,y,z) = ~ c(x,y,z) ~~ holds. Referring the curve to a suitable parameter t (or denoting the common ratio in (4.3) by dt) we can write the condition defining characteristic curves in the more familiar form of a system of ordinary differential equations ':;; = a(x,y,z), • dt =b(x,y,z), : =c(x,y,z). (4.4) The system is "autonomous" (the independent variable t does not appear explicitly). The choice of the parameter t in (4.4) is artificial. Using any other parameter along the curve amounts to replacing a,b,c by proportional quantities, which does not change the characteristic curve in xyzspace or the P.D.E. (4.2). Assuming that a,b,c are of class C' in a region n, we know from the theory of O.D.E.s that through each point of n there passes exactly one characteristic curve. There is a 2-parameter family of characteristic curves in xyz-space (but a 3-parameter family of solutions (x(t),y(t),z(t» of (4.4), since replacing the independent variable t by t+c with a constant c changes the solution (x,y,z), but not the characteristic curve, which is its range). If a surface S: z = u(x,y) is a union of characteristic curves, then S IS an integral surface. For then through any point P of S there passes a characteristic curve 'Y contained in S. The tangent to 'Y at P necessarily lies in the tangent place of S at P. Since the tangent to 'Y has the characteristic 9 1 The single first-order equation direction, the normal to S at P is perpendicular to the characteristic direction, which makes S an integral surface. Conversely we can show that every integral surface S is the union of characteristic curves, or that through every point of S there passes a characteristic curve contained in S. This is a consequence of the following theorem: Theorem. Let the point P = (xo,Yo, zo) lie on the integral surface z = u( x,y). Let y be the characteristic curve through P. Then y lies completely on S. PROOF. Let y given by (x(t),y(t),z(t» be the solution of (4.4) for which (x,y,z) = (xo,yo,zo) for t=to. From y and S we form the expression U=z(t)-u(x(t),y(t))= U(t). (4.5) Obviously U(to) =0 since P lies on S. By (4.4) dU = dz dt dt - uxCx(t),y(t) ) dx dt -Ily ( x(t),y(t)) dy dt = c(x,y,z) - uxCx,y )a(x,y,z) -Ily(x,y,z)b(x,y,z). This can be written as the ordinary differential equation ~~ =c(x,y, U+ u(x,y))-ux(x,y)a(x,y, U+ u(x,y)) -Ily(x,y)b(x,y, U+ u(x,y)) (4.6) for U, where for x,y we have to substitute the functions x(t),y(t) from the description of y. Now U=O is a particular solution of (4.6), since u(x,y) satisfies (4.2). By the uniqueness theorem for O.D.E.s, this is the only solution vanishing for t = to. It follows that the function U (t) defined by (4.5) vanishes identically. But that just means that the whole curve y lies on S. D As a consequence of the theorem two integral surfaces that have a point P in common intersect along the whole characteristic curve y through P. Conversely if the integral surfaces S \ and S2 intersect, without touching, along a curve y, then y is characteristic. For consider the tangent planes '17\,'172 to S\,S2 at a point P of y. Each of the planes has to contain the characteristic direction (a,b,c) at P. Since '17\ =1='172 it follows that the intersection of '17\ and '172 has the direction (a,b,c). Since the tangent T to y at P also has to belong to both '17\ and '172' it follows that T has the direction (a,b,c), and hence that y is characteristic. S. The Cauchy Problem for the Quasi-linear Equation We now have a simple description for the general solution u of (4.2): The integral surface z = u(x,y) is the union of characteristic curves. To get a better insight into the structure of the manifold of solutions it is desirable to have a definite method of generating solutions in terms of a prescribed lO 5 The Cauchy Problem for the Quasi-linear Equation set F of functions, called "data." Ideally we have a mapping F~u of data F onto solutions u of the P.D.E. The space of solutions is then described by the usually simpler space of data. A good deal of the theory of P.D.E.s is concerned with the "problem" of actually finding the u belonging to a given F. (Here "finding" commonly is equated with "establishing existence.") A simple way of selecting an individual u(x,y) out of the infinite set of all solutions of (4.2) consists in prescribing a curve r in xyz-space which is to be contained in the integral surface z = u(x,y). Let r be represented parametrically by (5.1) x= f(s), y=g(s), z=h(s). We are asking for a solution u(x,y) of (4.2) such that the relation > h(s) = u(j(s),g(s») (5.2) holds identically in s. Finding the function u(x,y) for given dataf(s), g(s), h(s) constitutes the Cauchy problem for (4.2). Actually the same curve r has many different parametric representations (5.1) for different choices of the parameter s. Introducing a different parameter (1 by a substitution s=q,«(1) will not change the solution u(x,y) of the Cauchy problem. We shall be satisfied here with a local solution u of our problem, defined for x,y near values Xo = f(so), Yo = g(so). In many instances the variable y will be identified with time and x with position in space. It is then natural to pose the problem of finding a solution u(x,y) from its initial values at the time y =0: (5.3) This initial-value problem obviously is the special Cauchy problem in which the curve r has the form (5.4) z = h(s), y=O, x=s, that is, r lies in the xz-plane and is referred to x as parameter. We notice that in the initial-value problem we prescribe a single function h(x), which in tum is determined uniquely by u, whereas in the general Cauchy problem many space curves r are bound to lead to the same u. An integral surface contains many curves r but only one intersection with the x~­ plane. Let then the functions f(s), g(s), h(s) describing r be of class C l in a neighborhood of a value so. Let u(x,O)=h(x). Po = (xo,yo,zo) = (j(so),g(so),h(so». (5.5) Assume that the coefficients a(x,y,z), b(x,y,z), c(x,y,z) in (4.2) are of class C I in x,y,z near Po. It is clear intuitively that the integral surface z = u(x,y) passing through r will have to consist of the characteristic curves passing through the various points of r. Accordingly we form for each s near So that solution x=X(s,t), y= Y(s,t), z=Z(s,t) (5.6) 11 1 The single first-order equation of the characteristic differential equations (4.4) which reduces to j(s),g(s),h(s) for t=O. The functions X, Y,Z then satisfy X,=a(X,Y,Z), ~=b(X,Y,Z), Z,=c(X,Y,Z) (5.7) identically in s, t and also satisfy the initial conditions X(s,O)=j(s), Y(s,O)=g(s), Z(s,O)=h(s). (5.8) From the general theorems on existence and on continuous dependence on parameters of solutions of systems of ordinary differential equations it follows that there exists a unique set of functions X(s,t), Y(s,t), Z(s,t) of class C 1 for (s,t) near (so,O) which satisfy (5.7), (5.8). Equations (5.6) represent a surface~: z=u(x,y) referred to parameters s, t if we can solve the first two equations for s, t in terms of x,y, say in the forms=S(x,y), t=T(x,y). Then the u defined by 7. = u(x,y) = Z(S (x,y), T(x,y» will be the explicit representation of xo=X(so,O), ~. (5.9) By (5.5), (5.8) Yo= Y(so,O). (5.10) Now the implicit function theorem asserts that we can find solutions s=S(x,y), t= T(x,y) of x=X(S (x,y), T(x,y», of class C1 y = Y(S(x,y), T(x,y» (5.11) in a neighborhood of (xo,Yo) and satisfying So= S (xo,Yo), 0= T(xQoYo), provided the Jacobian Ys(so,O) Yt(so,O) I (5.12) (5.13) does not vanish. By (5.7), (5.8) this amounts to the condition J= I j'(so) a(xo,yo,zo) g'(so) b(xo,yo,zo) I~O. (5.14) Thus (5.13) guarantees that locally (5.6) represents a surface ~: z = u(x,y). That ~ is an integral surface is clear in the parametric representation (5.6). For at any point P the quantities X" Y" Zt give the direction of the tangent to a curve s = const. on ~, which will have to lie in the tangent plane of ~ at P. Thus (5.7) shows that the tangent plane at any point contains the characteristic direction (a,b,c), and hence that ~ is an integral surface. [One can also verify analytically that the function u represented by (5.9) satisfies the differential equation (4.2) by first expressing ux,lly in terms of Sx' Sy, Tx, r;" and then expressing those four quantities in terms of Xs'X" Ys' Y, using (5.11).] This completes the local existence proof for the solution of the Cauchy problem, under the assumption (5.13). Uniqueness follows from the theorem on p. 10: Any integral surface through r would have to contain the 12 5 The Cauchy Problem for the Quasi-linear Equation characteristic curves through the points of f, hence would have to contain the surface represented parametrically by (5.6), and hence locally would have to be identical with the surface. Condition (5.14) is essential for the existence of a Cl-solution u(x,y) of the Cauchy problem. For if J=O we would find from (5.2), (4.2) that at s = so' x = f(so), y = g(so) the three relations bf'-ag'=O, (5.15) h'= f'ux + g'~, hold. These imply that bh' - cg' = 0, ah' - cf' =0 and hence thatf',g',h' are proportional to a,b,c. Hence J=O is incompatible with the existence of a solution unless f happens to be characteristic at so. Incidentally the Cauchy problem will have infinitely many solutions for a characteristic curve f, which are obtained by passing any curve f* satisfying (5.14) through a point Po of f and solving the Cauchy problem for f*. In the special case of a linear P.D.E. we can write (4.2) in the form a (x,y)ux + b(x,y)~ = c(x,y)u + d(x,y). (5.16) Here the system of three characteristic O.D.E.s reduces to the pair dx dy (5.17) dt =a(x,y), dt =b(x,y) or even to the single equivalent equation dy b(x,y) dx = a(x,y) . (5.18) Equations (5.11) or (5.18) determine a system of curves in the xy-plane, called characteristic projections, (also, more commonly and confusingly, just "characteristics") which are the projections onto the xy-plane of the characteristic curves in xyz-space. The characteristic curve is obtained from its projection x(t),y(t) by finding z(t) from the linear O.D.E. : = c{x(t),y(t»z + d(x(t),y(t». (5.19) We indicate how to proceed in the more general case of a quasi-linear equation for a function u = u(x l , ... ,xn) of n independent variables. Such an equation has the form n L ai(xI,···,Xn,u)U",,=C(XI,··.,Xn,u). (5.20) i= I Here the characteristic curves in XI ••• xnz-space are given by the system of O.D.E.s dx. (5.2Ia) d: =ai(xI'···'xn,z) fori=I, ... ,n : =c(xl,···,xn,z). (5.2Ib) 13 1 The single first-order equation In the Cauchy problem we want to pass an integral surface z=u(Xt, ... ,xn) in ~.n+ t through an (n - I)-dimensional manifold r given parametrically by Xj for i= l, ... ,n = ./;{St, ... ,sn-t) (5.22a) z=h{st"",sn_t). (5.22b) For that purpose we pass through each point of r with parameters St"",sn-t a characteristic curve (solution of (5.2Ia, b) reducing to (jt, ... ,jn,h) for t=O) rep~esented by for i= l, ... ,n xj=Xj{St, ... ,sn_t,t) (5.23a) z=Z{st>""sn_t,t). (5.23b) These equations form a parametric representation for the desired integral surface z = u(x t, ... , xn), provided relations (5.23a) can be solved for St, ... ,Sn-t, t. This is the case when the Jacobian ait aS t ain aS t ait aSn_ t at ain aSn- t an (5.24) J= does not vanish. 6. Examples (1) (See Section 2.) Uy + cux=O (6.1a) (c=const.) u{x,O)= hex). The initial curve r corresponding to (6.lb) is given by x=s, y=O, (6.1b) z=h{s). The characteristic differential equations are dx -=c dt ' dy -=1 dt ' dz =0 dt . (6.2) This leads to the parametric representation x=X{s,t)=s+ct, y= Y{s,t)=t, z=Z{s,t)=h{s) (6.3) for the integral surface. Eliminating s, t we find for the solution of the initial-value problem (6.1a, b) the representation z=h{x-ct) in agreement with (3.3). 14 (6.4) 6 Examples (2) Euler's P.D.E. for a homogeneous function u(xl, ... ,xn ): (a = const.=t=O). (6.5) Since equation (6.5) is singular at the origin (the J defined by (5.24) cannot be different from 0) we postulate the initial-value problem U(XI, ... ,Xn _ l , 1)= h(xl, ... ,xn _ l ) corresponding to a curve r (6.6) given by fori=I, ... ,n-l for i= n (6.7) z = h(sl' ... ,Sn-I). Solving the characteristic differential equations dXi (j[=Xi (6.8) fori=I, ... ,n dz dt =az leads to for i= 1, ... ,n-l .for i= n (6.9) and thus to (6.10) The solution U satisfies the functional equation u(Ax I ,·." Axn) = i\ "u (XI' ... , xn) (6.11) for any i\ > 0, and thus is a homogeneous function of degree a. For a < 0 the solutions of (6.5) generally become singular at the origin. More precisely the only solution U of (6.5) of class C I in a neighborhood of the origin is u=O. For along any ray i= 1, ... ,n from the origin referred to a parameter t we have by (6.5) du -d t ~ = £.J k= I CkUXk ( clt, ... ,cnt) a = -u. t Hence ut- a is constant along the ray, and thus u tends to 00 for t~O, unless u vanishes identically along the ray. We have here an example of a P.D.E. that has only a single solution if we restrict the domain of the solution to be a set containing the origin. 15 1 The single first-order equation (3) The solution u = u(x,y) of the quasi-linear equation (see [6]) (6.12) Uy+uux=O can be interpreted as a velocity field on the x-axis varying with the time y. Equation (6.12) then states that every particle has zero acceleration, and hence constant velocity. Let (6.13) u(x,O)= hex) describe the initial velocity distribution, corresponding to the manifold r in xyz-space given by (6.14) y=O, z=h(s). x=s, The characteristic differential equations dx dt =z, dy dt =1, dz =0 dt (615) . combined with the initial condition (6.14) for t=O lead to the parametric representation (6.16) z=h(s) y=t, x=s+zt, for the solution z=u(x,y) of (6.12), (6.13). Eliminating s,t from (6.16) yields the implicit equation u=h(x-uy) (6.17) for u as a function of x,y. (Notice the analogy to (6.4)!) The characteristic (projection) Cs in the xy-plane passing through the point (s,O) is the line x=s+h(s)y (6.l8a) along which u has the constant value u=h(s). (6.18b) Physically (6.18a) for a fixed s represents the path of the particle located at x = s at the time t = O. Now two characteristics CS1 and CS2 intersect at a point (x,y) with (6.19) If the y in (6.19) is defined, the function u must take the distinct values h(sl) and h(S2) at (x,y) and hence cannot be univalued. There always exist positive y of the form (6.19), unless h(s) is a nondecreasing function of s. For all other h(s) the solution u(x,y) becomes singular for some positivey. (Physically a particle with a higher velocity will eventually collide with one ahead of it having a lower velocity). In particular, u is bound to become singular if the initial velocity distribution h has compact support, except in the trivial case where h(s)=O. The nature of the singularity becomes clearer when we follow the values of the derivative uAx,y) along the 16 6 Examples characteristic (6.18a). We find from (6.17) that h'(s) u= x Hence for h'(s) <0 we find that I +h'(s)y (6.20) . becomes infinite at the positive time -I (6.21) y= h'(s)" Ux The smallest y for which this happens corresponds to the value s = So at which h'(s) has a minimum. At the time T= -1/h'(sJ the solution u experiences a "gradient catastrophe" or "blow-up:' There cannot exist a strict solution u of class C 1 beyond the time T. This type of behavior is typical for a nonlinear partial differential equation. It is possible, however, to define weak solutions of (6.12), (6.13) which exist beyond the time T. For that purpose (6.12) has to be given a meaning for a wider class of functions u that do not necessarily lie in C 1 or even are continuous. We can write (6.12) in divergence form aR(u) + as(u) =0 ay ax ' (6.22) where R(u), S(u) are any functions for which S'(u)= uR'(u). Relation (6.22) implies for any a,b,y the "conservation law" d 0= dy fba R (u(x,y»dx+ S(u(b,y»- S(u(a,y». (6.23) (6.24) Conversely (6.22) follows from (6.24) for any u Eel. Now (6.24) makes sense for more general u and can serve to define "weak" solutions of (6.22). In particular we consider the case where u is a C I-solution of (6.22) in each of two regions in the xy-plane separated by a curve x = ~(y), across which the value of u shall undergo a jump ("shock"). Denoting the limits of u from the left and right respectively by u- and u+, we find from (6.24) for a<~(y)< b O=S(u(b,y»-S(u(a,y»+ ~ (iIiR(u)dx+ ~bR(U)dx) = S(u(b,y»- S(u(a,y»+f R (u-)-f R (u+) _jliaS(u) dx- [baS(U) dx ax ax Ii = -(R (u+)- R (u-»f - S(u-)+ S(u+). a Hence we find the relation ("shock condition") d~ dy = S(u+)- S(u-) R(u+)-R(u-) (6.25) 17 I The single first-order equation connecting the speed of propagation dV dy of the discontinuity with the amounts by which Rand S jump. We observe that (6.25) depends not only on the original partial differential equation (6.12) but also on our choice of the functions R ( u), S (u) satisfying (6.23). PROBLEMS 1. Solve the following initial-value problems: (a) ux+~=U2, u(x,O)=h(x) (b) ~=xuux' u(x,O)=x (Answer: x=ue-YU implicitly.) (c) xux+y~+uz=u, u(x,y,O)=h(x,y) (d) x~-yux=u, u(x,O)=h(x) (Answer: u=hCV x 2+y2 )earctan<y/x).) 2. (Picone). Let u be a solution of a(x,y)ux+b(x,y)Uy= -u of class C l in the closed unit disk U in the xy-plane. Let a(x,y)x+b(x,y)y >0 on the boundary of U. Prove that u vanishes identically. (Hint:· Show that maxu,,;O, minu~O.) !l !l 3. Let u be a C I-solution of (6.12) in each of two regions separated by a curve x = €(y). Let u be continuous, but Ux have a jump discontinuity on the curve. Prove that d€ dy =u and hence that the curve is a characteristic. (Hint: By (6.12) (~+ -:- ~-) + u(ux+ - u;) =0. Moreover u(€(y ),y) and (d/ dy )u(€(y ),y) are continuous on the curve.) 4. Show that the function u(x,y) defined for y ~ 0 by u= -Hy+ \l3x+y2) for4x+y2>0 u=o for4x+y2<0 is a weak solution of (6.22) for the choice R(u)=u,S(u)=tu2. S. Define a weak solution u(x,y) of (6.22) as a function for which the relation (6.26) holds for any function </>(x,y) of class qr> (Relation (6.26) follows formally from (6.22) by integration by parts.) Show that this definition of weak solution also leads to the jump condition (6.25). 6. Show that the solution u of the quasi-linear partial differential equation ~+a(u)ux=O 18 (6.27) 7 The General First-order Equation for a Function of Two Variables with initial condition u(x,O)=h(x) is given implicitly by u=h(x-a(u)y) (6.28) Show that the solution becomes singular for some positive y, unless a(h(s» is a nondecreasing function of s. 7. The General First-order Equation for a Function of Two Variables The general first-order partial differential equation for a function z = u(x,y) has the form F(x,y,z,p,q) =0, (7.1) where p=ux,q=Uy. We assume that F where considered has continuous second derivatives with respect to its arguments x,y,z,p,q. Surprisingly enough the problem of solving the general equation (7.1) reduces to that of solving a system of ordinary differential equations. This reduction is suggested by the geometric interpretation of (7.1) as a condition on the integral surface z=u(x,y) in xyz-space determined by a solution u(x,y). The geometry here is more involved than in the quasi-linear case where we were concerned principally with integral curves. We shall have to deal with more complicated geometric objects, called "strips." Equation (7.1) can be viewed as a relation between the coordinates (x,y,z) of a point on an integral surface and the direction of the normal of the integral surface at that point, described by the direction numbers p,q, -1. An integral surface passing through a given point Po=(xo,yo,zo) must have a tangent plane z-zo=p(x-xo)+q(y-yo) (7.2) for which the direction numbers (p,q, -1) of the normal satisfy F(xo,yo,zo,p,q) =0. (7.3) Thus the differential equation restricts the possible tangent planes of an integral surface through Po to a one-parameter family. In general* such a one-parameter family of planes through Po can be expected to envelop a cone with vertex Po, called the Monge cone at Po (Figure 1.3). Each possible tangent plane touches the Monge cone along a certain generator. In this way the partial differential equation (7.1) defines afield of cones. A • surface z = u (x,y) is an integral surface if at each of its points Po it touches the cone with vertex Po. (See Figure 1.4.) In that case the generator along which the tangent plane touches the cone defines a direction on the surface. These "characteristic" directions are the key to the whole theory of integration of (7.1). In the special case of a quasi-linear equation (4.2) the Monge cone at Po degenerates into the line with direction (a,b,c) through Po. * For the present heuristic considerations we dispense with rigor. 19 1 The single first-order equation Figure 1.3 Figure 1.4 The central notion here is that of the envelope of a family of surfaces SA z= G(X,y,A) (7.4) depending on a parameter A. We combine (7.4) with the equation 0= GA (x,y, A). (7.5) For fixed A equations (7.4), (7.5) determine a curve 'lA. The envelope is the union of these curves. Its explicit equation is obtained by solving (7.5) for A in the form A= g(x,y) and substitution into (7.4): z=G(x,y,g(x,y»). (7.6) The envelope E touches the surface SA along the curve YA• For in a point (x,y,z) of YA we have g(X,y)=A, so that (7.6) holds; moreover by (7.5) the direction numbers of the normal of E are (Gx + GAgx , Gy + GAgy ' -1)= (Gx,Gy ' -1), the same as for SA. It is often advantageous to write equations (7.4), (7.5) for a fixed A in the form of differential equations 0= G7I.x dx + GAY dy (7.7) satisfied along the curve YA• Now for fixed xo,yo,zo, equation (7.2) defines a one-parameter family of planes, where we can choose p as the parameter and think of q as expressed in terms of p from (7.3). By (7.7) the generator along which the plane touches the Monge cone satisfies the equations dq (7.8) dz=pdx+qdy, O=dx+ dp dy. Since by (7.3) (7.9) 20 7 The General First-order Equation for a Function of Two Variables the direction of the generator is given by dz=pdx+qdy, dx=dy F;, Fq • (7.10) On a known integral surface S: z=u(x,y) equations (7.10) define a direction field, since F;,(x,y,u,ux,zs,), Fq(x,y,u,ux'zs,) are then also known functions of x,y. We define the characteristic curves belonging to the integral surface S as those fitting the direction field. Using a suitable curve parameter t, the characteristic curves on S are given by the system of ordinary differential equations dy dx (7.10a) dt = Fq(x,y,z,p,q) dt = F;, (x,y,z,p,q), dz dt = pF;, (x,y,z,p,q) + qFq (x,y,z,p,q), (7.10b) where z=u(x,y), p=uxCx,y), q= zs,(x,y). (7.11) It is clear that for a quasi-linear equation (4.2) relations (7.10a,b) reduce to the characteristic differential equations (4.4). The main difference in the present more general case is that without the use of (7.11), that is, without the knowledge of the integral surface S, equations (7.lOa,b) form an underdetermined system for the five functions x,y,z,p,q of t. However, the system is easily completed by two further equations. Partial differentiations with respect to x,y of the P.D.E. F(x,y, u(x,y), uxCx,y), zs, (x,y» =0 (7.12) furnish the relations Fx + ux~ + uxxF;, + uxyFq=0 (7.13a) F;, + zs,Fz + uxyFp + ~Fq=O. (7.13b) Then along a characteristic curve on S we have by (7.11), (7.lOa) dx dy dt = uxx dt + Uxy dt = uxxF;, + uxyFq = - Fx - uxFz dp with a similar relation for dqj dt. Writing these relations in the form dp = - FxCx,y,z,p,q) - pFzCx,y,z,p,q) (7.14a) dq dt = -F;,(x,y,z,p,q)-qFzCx,y,z,p,q) (7.14b) dt relations (7.lOa,b), (7.14a,b) constitute an autonomous system of five ordinary differential equations for the five functions x,y,z,p,q of t, which does not require knowledge of the integral surface z = u(x,y) for its formulation. 21 1 The single first-order equation The expression F(x,y,z,p,q) is an "integral" of the system, that is, F is constant along any solution, since by (7.lOa,b), (7.14a,b) ~ ~ ~ ~ ~ ~ dt=~~+Ey~+~~+~~+~~ =Fx~+EyFq+Fz(p~+qFq)+~( -Fx-p~)+Fq( -Ey-qFz)=O. Hence along any trajectory of the system we have F=O for all t, if F=O for some particular t. We refer to the system of five ordinary differential equations (7.lOa,b), (7.14a,b), together with the dependent relation F(x,y,z,p,q)=O (7.15) as the characteristic equations. A solution of the characteristic equations is a set of five functions x(t),y(t),z(t),p(t),q(t). Generally we call a quintuple (x,y,z,p,q) a plane element and interpret it geometrically as consisting of a point (x,y,z) and of a plane through the point with equation r - z=p(~- x)+ q('Ij - y) (7.16) in running coordinates ~,'Ij,r. Then p,q, -1 are direction numbers of the normal of the plane. An element is called characteristic if it satisfies (7.15). A one-parameter family of elements (x(t),y(t),z(t),p(t),q(t» is called a strip if the elements are tangent to the curve formed by the points (x(t),y(t),z(t», the support of the strip. For that to be the case, the strip condition (7.17) has to be satisfied. A solution of the characteristic equations will be called a characteristic strip. (Here the strip condition holds in consequence of relations (7.lOa,b).) (See Figure 1.5.) A surface z=u(x,y) referred to parameters s,t can be thought of as consisting of a two-parameter family of elements (x(s, t), z(s,t),p(s,t), q(s,t» formed by the points of the surface and the corresponding tangent planes. Not every two-parameter family of elements. forms a surface. It is necessary again that dz=pdx+q~ Figure 1.5 22 (7.18) 8 The Cauchy Problem holds along the family, i.e., that the strip conditions az _ ax + ay as -Pas q as' az _ ax at -Pat + ay qat () 7.19 are satisfied. Visualizing an element as a small piece of plane attached to a point, the elements of a two-parameter family belonging to a surface have to fit together smoothly somewhat like scales on a fish. As a solution of a system of ordinary differential equations a characteristic strip is determined uniquely by anyone of its elements. If that element of the strip consists of a point P of an integral surface S and of the tangent plane to S at P, then the strip is made up of the characteristic curve of S through the point P and of the tangent planes of S along that curve. If another integral surface touches S in the point P then that surface will also touch S all along the characteristic curve. Equations (7.lOa,b), (7.14a,b) describe a "law of propagation" of characteristic elements or of tangent planes on an integral surface along characteristic curves. A lower-dimensional geometric interpretation often is useful. We associate with (x,y,z,p,q) a "line element" in the xy-plane consisting of the point (x,y) and the line O=p(g-X)+q(l1-Y) (7.20) in running coordinates g,l1. The line (7.20) is the level line r = z of the plane (7.16). The geometric line element does not determine x,y,p,q uniquely, since p and q can be replaced by any proportional numbers. A characteristic strip gives rise to a family of line elements. Using z instead of t as a parameter, the line elements "propagate" for varying z in a definite way described by the equations F;, dx dz = pF;, + qFq , dp dt Fx+pFz = - pF;,+qFq ' dy dt Fq = pF;, + qFq dq ~+qFz dt = - pF;, + qFq . (7.2Ia) (7.2Ib) We can start out with an initial line element (xo,yo,Po,qo) for z = Zo (in which Po, % are to be replaced by proportional quantities so that F(xo,yo,zo,Po,%) =0 (7.22) holds). With changing z the line element moves along the curve x = x(t), y = yet) (called a "ray"). The line elements are not tangent to the ray (no "strip condition"), since generally dx dy p dt +q dt =pF;,+qFq=l=O. 8. The Cauchy Problem The Cauchy problem for (7.1) consists in passing an integral surface through an "arbitrary" initial curve r given parametrically in the form x=j(s), y=g(s), z=h(s). (8.1) 23 1 The single first-order equation This will be achieved by passing suitable characteristic strips through r. We assume thatj,g,h are of class C 1 for s near a value So corresponding to a point (S.la) We first have to complete r into a strip consisting of characteristic elements. That is, we have to find functions p=</>(s), (S.2) q=t/l{s) such that h'(s) = </>(s)f'(s) + I/I(s) g'(s) (S.3a) F(j(s),g(s),h(s),</>(s), 1/1 (s)) =0. (S.3b) Since equation (S.3b) is nonlinear there may be one, or several, or no solution (</>,1/1) of (S.3a,b). We assume that we are given a special solution Po>qo of (S.4) such that d= j'(so)Fq (xo,yo,zo,Po, qo) - g'(so).F;. (xo>yo,zo,Po,qoh=O. (S.5) That is, we have found a characteristic plane tangent to r at Po such that the generator of contact between the plane and the Monge cone at Po has a different projection onto the xy-plane than the tangent to r at Po. By the implicit function theorem there exist then unique functions <P(s), 1/1 (s) of class C 1 near so' satisfying (S.3a,b) and reducing to Po>qo for s=so. Through each element (f(s),g(s),h(s),<p(s),I/I(s» we now pass the characteristic strip reducing to that element for 1=0. In this way we find five functions x=X(s,/), y= Y(s,/), z=Z(s,t), p=P(s,t), q=Q(s,t) (S.6) defined for Is-sol and It I sufficiently small, which satisfy for fixed s the differential equations (7.1Oa,b), (7.14a,b) as functions of t, and for s=o reduce respectively to j(s),g(s), h(s), <p(s), 1/1 (s). The relation F(X, Y,Z,P,Q)=O (S.7) holds identically in s,t, since it holds for t=O by (S.3b). From what preceded it is clear that if there exists an integral surface S through r containing the element (xo,yo,zo,Po>qo), then that surface must be the union of the supports of the characteristic strips we constructed. In particular, the first three equations in (S.6) must constitute a parametric representation for S. Conversely we shall prove that (S.6) represents a solution of our Cauchy problem in parametric form in a neighborhood of the point Po. First of all we can solve the first two equations (S.6) for s, t in terms of x,y for (x,y) 24 8 The Cauchy Problem near (xo,Yo). For by (8.la) Xo= f(so)=X(so,O), yo=g(so) = Y(so,O) and we have a nonvanishing Jacobian at s=so, 1=0: a (x,y) /Xs a (s,1 ) = xt (8.7a) Substituting into the third equation (8.6) yields an explicit equation z = u(x,y) for a surface passing through r. By (8.7) this will be an integral surface, if we can show that the p,q defined by the last two equations (8.6) are identical with Ux and ~. Now from the first three equations in (8.6) we can determine Ux ' zs, uniquely in terms of s,1 by the chain rule which yields the relations Zs = uxXs + zs, Ys' Zt = uxXt + uy y, (8.8) We have proved that ux=P(s,/), zs,=Q(s,/), (8.9) if we can verify the identities Zs = PXs + QYs, Zt = PXt + QY,. (8.10) These equations just express that the two-parameter family of elements (8.6) belongs to a surface. The second equation in (8.10) is a consequence of the characteristic differential equations (7.lOa,b) satisfied by X, Y,Z, P, Q, as functions of I. To verify the first equation we introduce the expression (8.11) Here A (s,O) = h' -cf>f' - t[;g' =0 (8.12) by (8.3a). Moreover, making use of the characteristic equations for X, Y,Z,P,Q, we have At = Zst - PtXs - Qt Ys - PXst - QYst a = as (Zt - PXt - QYt)+PsXt + QsYt - Qt Ys - PtXs =PsF;,+ QsFq+Xs(Fx+ FzP)+ Ys(r;. + FzQ) = aF as -~(Zs-PXs- QYs )= -~A. (8.13) But then, by integration, A (S,/)=A(s,O)exp( - fotFzdl) =0 because of (8.12). This completes the local existence proof for a solution of the Cauchy problem under the assumption that we have a solution Po, qo of (8.4), (8.5). 25 1 The single first-order equation The same methods apply to first-order equations in more independent variables. The general equation for a function u(x" ... ,xn ) has the form F(x" ... ,xn,z,p" ... ,Pn)=O, (S.14) where z = u, Pj = Ux .' The Cauchy problem here consists in finding an integral surface iIi. x, ... xnz-space that passes through an (n -1)dimensional manifold r given parametrically by z=h(s",,,,sn_')' X j = /;(s",,,,sn_') for i= l, ... ,n. This is achieved as before by passing through each point P of r a characteristic strip tangent to r at P. We first complete r into a strip by finding functions pj = q,j(Sj, ... ,sn-') for which ah ~ afk a-= ~q,kaSj k=' Si . forl=l, ... ,n-l (S.14a) (S.14b) in analogy to (S.3a,b). A characteristic strip here is a set of "elements" (x" ... ,xn'z,p" ... ,Pn) depending on a parameter t that satisfies in addition to (S.14) the system of ordinary differential equations dXj di = F;", dz dt = tipj dt = - Fx , - FzPj for i= 1, . .. ,n n .~ PiF;,,' (S.15a) (8.15b) 1= , For existence assumption (8.7a) here has to be replaced by a= aft as, afn as, aft asn_, afn asn_, F;" F;,n ~O at one point of r. An instructive example is given by the equation C2(p2 + q2) = 1 (8.l5c) (8.16) (c = const. > 0), which arises in geometric optics. There the level lines of a solution u are interpreted as "wave fronts," marking the location to which light has spread. (We shall obtain the same lines as lines of discontinuity for solutions of the wave equation.) Geometrically (8.16) states that tangent planes of an integral surface make a fixed angle O=arctanc with the z-axis. The Monge cone enveloped by possible tangent planes through a point is then a circular cone with opening angle 20. 26 8 The Cauchy Problem For convenience we write (S.16) as F=Hc7;2+ C2q2-1)=0 (S.17) leading to the characteristic equations dx =c2.. P, dt ~~ dy =c2q dt ' = C2(p2+ q2)= I, dp dt dq dt -=-=0 . (S.IS) A given initial curve r: z=h(s) (S.19) is completed into a strip by choosing p=cp(s),q=l/I(s) according to the equations x=f(s), y=g(s), h'(s) = cp(s )f'(s) + l/I(s) g'(s), (S.20) 2 These equations have no real solution when j'2 + g,2 < c h'2, that is, when r forms an angle less than 0 with the z-axis (f is "timelike"). For a "spacelike" r with j'2 + g,2 > c2h,2 we can solve (S.20) in two different ways, giving rise to two different solutions of the Cauchy problem. Of special interest is the case where r is the intersection x=f(s), y=g(s), Z=O (S.21) of the integral surface z = u(x,y) with the xy-plane. For this space-like r there are two solutions (cp(s),l/I(s» of O=cpf' + l/Ig', cp2+l/I 2=C- 2, (S.22) differing only in sign. The characteristic strips with initial elements on r are given by (S.23a) y = g(s) + c2tl/1(s), x = f(s) + c2tcp(s), (S.23b) Z = t, P =cp(s), q=l/I(s). We represent the integral surface by its level lines in the xy-plane y/: u(x,y)=z=const.=t (S.24) interpreted as a "wave front" moving with the "time" t. Equations (S.23a) for fixed t give the curve y/ referred to the parameter s. We think of y/ as made up of line elements (x,y,p,q), i.e., of points (x,y) and corresponding tangents (S.25) p(~- x) + q(l1- y) =0. The elements propagate individually according to (S.23a,b) for fixed s. The point (x,y) moves along the ray (S.23a) with constant speed (: r+(: r =C~cp2+l/I2 =c. (S.26) The ray is the straight line of direction (cp,l/I)=(p,q), hence coincides at 27 1 The single first-order equation each point with the normal to the level line 'Yt. We see that the wave fronts 'Yt form a family of curves with common normals ("parallel" curves). Here 'Yt can also be obtained from 'Yo by laying off a fixed distance ct along each normal of 'Yo. Thus 'Yt is also the curve of constant "normal distance" ct from 'Yo' (The choice between "interior" or "exterior" normal directions corresponds to the choice between the two solutions of the Cauchy problem.) 9. Solutions Generated as Envelopes The envelope S of a family of integral surfaces SA of (7.1) with equation z= G{X,y,A) (9.1) is again an integral surface. This is obvious from the geometric interpretation of (7.1) and the fact that every tangent plane of the envelope is a tangent plane of one of the surfaces of the family. Here S touches SA along the curve given by the two equations z= G{X,y,A), 0= GA {x,y, A). (9.2) Since integral surfaces can touch only along characteristic strips, we see that completing equations (9.2) for fixed A by p=GAX,y,A), q=Gy{X,y,A) (9.3) describes a characteristic strip. We obtain its parametric representation with (x,y,z,p,q) as functions of some parameter t by solving the equation 0= GA (x,y, A) in some parametric form x = x (t),y = y(t) and substituting into the other equations. In this way a one-parameter family of solutions of the partial differential equation (7.1) yields a further solution and a one-parameter family of characteristic strips, purely by elimination. Using this observation we can obtain the "general" solution of (7.1) and the "general" characteristic strip from any special two-parameter family u= G{X,y,A,P.) (9.4) of solutions of (7.1). Many different one-parameter families are obtained from (9.4) by substituting for p. any function p. = w(A). Here for a particular A and a suitable function w the values of p. = w(A) and v = W'(A) are arbitrary. It follows that for general A, p., v the equations (9.4a) 0= GA (X,y,A,P.):t- vG,. (X,y,A,P.) z = G (x,y, A, p.), (9.4b) q= Gy (X,y,A,P.) p = GAX,y,A,P.), describe a characteristic strip. We obtain in this way the "general" characteristic strip containing an arbitrary characteristic element (xo,yepzepPo,qo)' We only have to determine A,P.,V in such a way that equations (9.4a, b) hold for x,y,z,p,q replaced by xo,Yo, Zo,Pep qo· These are essentially only 3 conditions for A,P., v since the equation F(x,y,z,p,q) =0 holds for all elements determined from (9.4a, b) as well as for the prescribed characteristic element. 28 9 Solutions Generated as Envelopes The Cauchy problem of finding an integral surface of (7.1) passing through a curve r can be solved directly with a knowledge of the two-parameter family (9.4). We only have to find a one-parameter subfamily of integral surfaces that touch r and then form their envelope. For r given by (8.1) this amounts to finding functions A=A(S), p.=p.(s) such that the relations h = F(j,g,A,P.), (9.5) h'= GAf,g,A,p.)f' + Gy (j,g,A,P.)g' hold identically in s. The solution is then determined by eliminating S from the equations u= G (X,y,A,P.), 0= GA (x,y,A,p.)N + G,. (X,y,A,P.) p.'. (9.6) Of special interest is the limiting case, when r degenerates into a point (xo,Yo,zO>. Taking the solutions (9.4) for which A,P. are such that Zo= G(Xo,yo,A,P.) and forming their envelope we obtain an integral surface with a conical singularity at (xo,yo,zo), called the "conoid" solution. The solution of the general Cauchy problem can be obtained by taking the envelope of the conoids that have their singularities on the prescribed curve r. Any two-parameter family of functions (9.4) determines a first-order partial differential equation (7.1) of which these functions are solutions. We only have to eliminate the parameters A, p. between the equations u=G(X,yA,P.), ux=GAx,y,A,P.), ~=Gy(x,y,A,p.). (9.7) For the resulting partial differential equation we can immediately find all characteristic strips and solve the Cauchy problem. An example is furnished by the equation c2(u;+u;)=1 (9.8) consider earlier. The equation has the special two-parameter family of linear solutions u= G (X,y,A,P.) = c-1(XCOSA+ ysinp.)+ p. (9.9) representing planes in xyz-space forming an angle O=arctanc with the z-axis. The general integral surface z = u(x,y) is the envelope of a oneparameter subfamily of the planes (9.9). The conoid with "vertex" or singular point (xo,yo,zo), here identical with the Monge cone, is the envelope of the planes (9.9) passing through (xo,yo,zo), i.e., of the planes z - Zo= c-1(x- Xo)COSA+(y - Yo)SinA). (9.10) The conoid thus is the circular cone (9.11) c2(z - zo)2 = (x - xoi + (y - YO)2. We can find the solution (9.8) passing through an initial curve "Yo in the xy-plane by forming the envelope of the conoids with vertex on "Yo. Since the level line z=const. of the conoid with vertex (xo,yo,O) is a circle of radius ct and center (xo,yo), we obtain the level line "YI of the envelope by 29 I The single first-order equation forming the envelopes of the circles of radius ct with centers on 'Yo' This agrees with the earlier representation of 'Yt as curve of normal distance ct from 'Yo. It corresponds to Huygens's generation of the wave front 'Yt as the envelope of "circular" waves issuing from the original wave front 'Yo. PROBLEMS 1. For the equation u;+u;=u 2 find (a) the characteristic strips; (b) the integral surfaces passing through the circle x=coss, y=sins, z= I [Answer: z=exp[±(I-Vx2+y2)]]; (c) the integral surfaces through the line x=s,y=O, z= 1 [Answer: u=exp(±y)]. 2. For the equation Uy = u; (a) find the solution with u(x,0)=2X 3/ 2 [Answer: u=2x 3/2(1-27y)-1/2]; (b) prove that every solution regular for all x,y is linear. 3. For the equation u = xUx + yUy + find a solution with u(x, 0) = HI - X2). Hu; + U;) 4. Given the family of spheres of radius I with centers in the xy-plane u= G(x,y,lI.,p.)=YI-(x-lI.i-(y- pi , find the first-order partial differential equation they satisfy. Find all characteristic strips and give a geometric description. Find the conoid solution with vertex (O,O,D. Find the integral surfaces through the line x=s,y=O, z=t. 5. (Characteristics as extremals of a variational problem). Consider for a given function H (Xl'''' ,Xm t'PI>'" ,Pn) the partial differential equation F= au +H (Xl,· .. ,xn,t, ax! au , ... , aXn au ) =0 at (Hamilton-Jacobi equation) for U=U(XI, ... ,Xmt). Obtain the characteristic equations in the form dxi dpi -=-H (ji=Hp" dt x,' Setting dXi / dt = Vi' du / dt = L we use the first n + I equations to express L as a function of XI,. .. ,xmt,vJ, ... ,vn. Show then that 4,=Pi' which implies that d dt 4 , -Lx,=O. These are the Euler-Lagrange equations for an extremal of the functional f L(xl> ... ,xmt,dxt/dt, ... ,dxn/dt)dt. 30 Second-order equations: hyperbolic equations for functions of two independent variables * 2 1. Characteristics for Linear and Quasi-linear Second-order Equationst We start with the general quasi-linear second-order equation for a function u(x,y): (1.1) auxx + 2buxy -+ CUyy = d, where a,b,c,d depend on x,y,u,ux,lly. Here the Cauchy problem consists of finding a solution u of (1.1) with given (compatible) values of u, ux' uy on a curve y in the xy-p1ane. Thus, for y given parametrically by x= f(s), y =g(s), (1.2) we prescribe on y u=h(s),. ux=cp(s), (1.3) The values of any function v(x,y) and of its first derivatives vAv,y, v/x,y) along the curve yare connected by the compatibility condition ("strip condition") dv (1.4) ds =vJ'(s)+Vyg'(s) which follows by differentiating v(f(s),g(s» with respect to s. Applied to the solution u of the Cauchy problem this implies the identity h'(s) =cp(s )f'(s) + 1{;(s )g'(s) (1.5) between the Cauchy data. Thus no more than two of the functions h, cp, 1{; * ([7], [13], [6]) t([22D 31 2 Second-order equations can be prescribed arbitrarily. Instead we might give on y the values of u and of its normal derivative: - u g' +Uy./' x X(s). (1.6) u=h(s), YJ'2+ g ,2 Compatibility conditions also hold for the higher partial derivatives of any function on y. Thus taking v = Ux or v = Uy we find that du ; = uxxf'(s) + uxyg'(s), dUy di= ux;1'(s) + lIyyg'(s). (1.7) Similar relations are valid for the s-derivatives of Uxx' uxy' Uyy' etc. If now u(x,y) is a solution of (Ll), (1.3) we have the three linear equations auxx + 2buxy + cUyy = d (1.8a) cp' (1.8b) f' Uxy + g' Uyy = \[;' (1.8c) f' Uxx + g' Uxy = for the values of uxx,uxy,Uyy along y, with coefficients that are known functions of s. These determine uxx,uxy,Uyy uniquely unless J' g' A= 0 a J' 2b 0 g' c = ag,2 - 2bJ' g' + CJ'2 = o. (1.9) We call the "initial" curve y characteristic (with respect to the differential equation and data), if A=O along y, noncharacteristic if A*O along y. Along a noncharacteristic curve the Cauchy data uniquely determine the second derivatives of u on y. As a matter of fact, we can then also find successively the values of all higher derivatives of u on y, as far as they ~xist. We obtain, e.g., three linear equations with determinant A for "xxx' uxxy , uxyy by differentiating (Ll) partially with respect to x, and using the two equations obtained from (1.4) for v = Uxx and v = uxy; the c.oefficients in the three equtions only involve the values of u and its first and second derivatives, known already. Obtaining in this way the values of all derivatives of u in some particular point (xo,yo) on y, we could write down a formal power series for the solution of the Cauchy problem in terms of powers of x - xo,y - Yo. It would be an actual representation of the solution u in a neighborhood of (xo,Yo), if u were known to be analytic. This procedure will be legitimized in the case of analytic Cauchy data, when we discuss the Cauchy-Kowalewski theorem below. In the case of a characteristic initial curve y, equations (l.8a, b, c) are inconsistent, unless additional identities are satisfied by the data. Hence the Cauchy problem with Cauchy data prescribed on a characteristic curve 32 2 Propagation of Singularities generally has no solution. Write condition (1.9) for a characteristic curve as a dy2 - 2b dx dy + Cdx 2= O. We can solve (LlO) for dy / dx in the form (LlO) dy = b± Yb 2 -ac (1.11) dx a When the characteristic curve y is given implicitly by an equation q,(x,y) = const., we have CPx dx + </y dy = 0 along y so that (Ll 0) reduces to the equation acp; + 2bcpx</y + ccp; = o. (Ll2) Relation (LlI) is an ordinary differential equation for y provided a,b,c are known functions of x,y. This is the case when either a fixed solution u= u(x,y) of (Ll) is considered, or when the equation (Ll) is linear, that is, a=a(x,y), b=b(x,y), c=c(x,y), d= - 2D(x,y )ux - 2E(x,y)~ - F(x,y)u - G(x,y). (1.13) The equation (1.1) is called elliptic if ac - b 2 > 0, hyperbolic if ac - b2 < 0, and parabolic if ac - b 2 = O. Restricting ourselves to the case of real variables, we observe that corresponding to the choice of ± in (LlI) there are two families of characteristic curves in the hyperbolic case, one in the parabolic case, and none in the elliptic case. We note, though, that in the nonlinear case, ,"type" (elliptic, parabolic, hyperbolic) is not determined by the differential equation, but can depend on the individual solution, and even for a linear equation might be different in different regions of the plane. 2. Propagation of Singularities The characteristic curves are closely associated with the propagation of certain types of singularities. Along a noncharacteristic curve the Cauchy data uniquely determine the second derivatives of a solution. One approach to defining "generalized" solutions of (1.1), not necessarily of class C 2, consists of considering solutions of class C l with second derivatives that have jump discontinuities along a curve y. More precisely. we assume that we have a certain region in the xy-plane divided by a curve y into two portions I and II. There shall be two solutions uI and uII of (1.1) respectively defined and of class C 2 in the closed regions I and II. uI and uII together define a function u in the union of I and II with discontinuities along y. The resulting u, pieced together ordinarily cannot be considered a "generalized" solution of (1.1), unless (1.1) in some generalized sense still holds on y. This requires certain tramition conditiom along y. The simplest to consider here is the case where the resulting u is required to be of class 33 2 Second-order equations C I, and hence the functions uI and u ll as well as their first derivatives coincide along y. If also the second derivatives coincide, u actually is a "strict" solution of class C 2 • Of interest, therefore, is the case where the second derivatives of uI and ull are not the same on y. Since however, by assumption u I and u ll have the same Cauchy data along y, a discontinuity in the second derivatives of u can only occur if y is a characteristic curve. We analyze the situation in more detail for a linear second-order equation 0= Lu= a(x,y )uxx +2b(x,y )uxy + c(x,y)Uyy +2d(x,y)ux +2e(x,y)~ + j(x,y)u (2.1) with regular coefficients a,b,c,d,e,j. Let y be a curve in the xy-plane given, say, by an equation x = <f>(y). (Precise regularity assumptions justifying what follows can easily be supplied by the reader. These are not relevant for the present discussion.) Let Sl be an open set in the xy-plane and y be an arc in. Sl such that Sl- y consists of two open disjoint sets I and II. We say that a function u defined in Sl has a jump discontinuity along y, if u = u I in I, u = UIl in II, where u I is continuous in 1+ y and u ll is continuous in 11+ y. We denote by (2.2) the jump of u at a point (<f>(y),y) of y. Then along y d dy [ u] = ( U;I(<f>(y ),y ) - u; (<f>(y ),y ) )<f>'(Y )+ ~I(<f>(y ),y ) - ~ (<f>(y ),y ) = [ux]<f>' + [uy J. In particular [u] = 0 when u is continuous along y, and thus (2.3) (2.4) We consider now the case where uI(x,y), uII(x,y) are of class C 3 and satisfy (2.1) respectively in 1+ y and II + y, defining a function u of class C l in Sl. Then [ u] = [ ux ] = [ ~ ] = o. (2.5) Moreover, subtracting (2.1) formed for u I and u ll along y yields a[ uxx ] + 2b[ uxy] + c[ Uyy] =0, (2.6) since a,b,c,d,e,j are continuous. From (2.5) we find that [ uxx ]<f>' + [ uxy] = 0, [ Uxy ]<f>' + [ Uyy] =0. (2.7) Hence for a C I-function u the jumps in the second derivatives are not independent. Knowing, for example, the jump of Uxx' those of uxy, Uyy are uniquely determined. Setting [Uxx]=A, we have [ uxx ] = A, 34 [ Uxy ] = - <f>'A, [ ~y ] = <f>,2A• (2.8) 3 The Linear Second-order Equation For a solution of the differential equation it follows now from (2.6) that a - 2bcp' + Ccp,2 = 0 (2.9) unless A=O, that is, unless uE C 2• Recalling that Cp'=dx/ dy, equation (2.9) asserts that 'Y is a characteristic curve. According to (2.8) the quantity A measures the "intensity" of the jumps in the second derivatives. We interpret y as the time, and cp as the point x = cp(y) moving along the x-axis. For every y we have in u(x,y) a function of x whose second derivative is discontinuous at the moving point cp(y). The speed dx / dt of "propagation of the discontinuity" is determined by (2.9). It is remarkable that the jumps in different points of 'Y are related to each other. There is a definite law according to which the intensity A of the jump propagates along 'Y. To find it we derive from (2.8) the relations A' = ':t = [uxxx ]cp' + [ uxxy ], - (CP'A)' = [uxxy ]cp' + [uxyy J. (2.10) In addition, differentiating (2.1) formed for uI and uII with respect to x and forming the jumps on 'Y, we find that 0= a [ uxxx ] + 2b [ uxxy ] + c [ uxyy] + ax [ uxx ] + 2bx [ uxy] + cx[ Uyy ] + 2d[ uxx ] +2e[ uxy] Eliminating the third derivatives, using (2.8) and (2.9), one arrives at the relation 0= 2( b - ccp')A' + (ax - 2bA' + cA,2 + 2d - 2ecp' - Ccp")A. (2.11) This is an ordinary differential equation for the jump intensity A, which regulates its growth during propagation. If, for example, A=O in one point of 'Y, it follows that A=O all along 'Y, so that no jump at all occurs. 3. The Linear Second-order Equation We analyze in more detail the linear second-order equation auxx+2buxy+c~ +2dux+2~+ ju=O (3.1) with coefficients a, b, c, d, e,j depending on x,y. Introducing new independent variables ~,1/ by the substitution, ~=CP(x,y), 1/=t/I(x,y), (3.2) we transform this linear equation into one of the same type, Lu=A(~,1/)u~E+2B(~,1/)ufrl+'" =0, (3.3) 35 2 Second-order equations where, A = act>; + 2bct>Ay + cct>; B = act>xo/x + b(ct>xo/y +ct>yl[;x) + c<lyl[;y (3.4) C = 01[;; + 2bl[;xo/y + cl[;; etc. This suggests, in the hyperbolic case, that one can simplify the differential equation by introducing the characteristics as new coordinate lines. Let ~=ct>(x,y) = const., 11 = I[;(x,y) = const. be the two families of characteristics in the xy-plane, so that both ct> and I[; satisfy (1.12). By (3.4) this implies that A = 0 and C = 0, and the hyperbolic equation reduces, after division by B, to the normal form, ue.., + 2Du~ + 2Eu." + Fu = O. (3.5) The new equation has the lines ~ = const. and 11 = const. as characteristic curves. By a further linear transformation, X'=~+l1, (3.6) Y'=~-l1, one can also transform (3.5) into the alternate form u.,,'y'- ux'x' +2D'ux' + 2E'u.", + F'u=O. (3.7) In the elliptic case, where ac - b2 > 0, there exist no real characteristics. We can attempt to find a real transformation (3.2) taking (3.1) into an equation of the form, u~~ + u."." + 2Du~ + 2Eu." + Fu = o. (3.8) This means we want to choose ct>(x,y),I[;(x,y), so that A = C, B=O. This can be achieved by taking for ct>, I[; solutions of the system of equations, ct>x = bl[;x + cl[;y W ' ct>y = - 01[;x + bl[;y W ' (3.9) where W = Vac - b2 • Eliminating ct> from (3.9) we see that I[; has to be a solution of the Beltrami equation, (3.10) EXAMPLE (The Tricomi Equation). Uyy - YUxx=O. (3.11) For this equation, ac - b2= - y. Hence for y < 0, ac - b2> 0, and the equation is elliptic. For y > 0, ac - b 2 is negative and the equation is hyperbolic. On the x-axis, it is parabolic. (See Figure 2.1.) Here, the characteristic equation (1.10) reduces to - yt(y2+ dx 2=0 or dx±Vy t(y=0 fory>O. 36 (3.12) 3 The Linear Second-order Equation y o x elliptic Figure 2.1 The characteristic curves in the half plane y > 0 are therefore 3x ± 2(y )3/2 = const. (3.13) The transformation, (3.14) ~=3x-2y3/2, reduces the equation to the normal form: I uE- u" (3.15) uE'I-'6 ~-1J =0. The curves 3x - 2y 3/2 = canst. are the branches of cubic cUrves having positive slope and -the--curves 3x + 2y 3/2 = canst. are the symmetric curves with negative slopes. On y = 0, the curves have cusps with a vertical tangent. PROBLEMS 1. For the equation of minimal surfaces (2.12), p. 3 of Chapter 1, find (a) all minimal surfaces of revolution about the z-axis (i.e., u = x 2 +y2 (b) the differential equations for the (imaginary) characteristic curves. In/ ) 2. Find by power series expansion with respect to y the solution of the initial-value problem ~=u",,+u u(x,O)=e", Uy(x,O) =0. 3. (Legendre transformation, Hodograph method). Let u(x,y) be a solution of a 37 2 Second-order equations quasi-linear equation of the form a(ux,uy)uxx +2b(ux ,uy )uxy + c(ux'~)uy'y =0. Introduce new independent variables ~=uAx,y), ~,1/ and a new unknown function If> by 1/=uy (x,y), If>=xux+Yuy-u. (3.16) Prove that If> as a function of ~,1/ satisfies x = If>~, Y = <Pr, and the linear differential equation (3.17) 4. The One-Dimensional Wave Equation The simplest of all hyperbolic differential equations is the one-dimensional wave equation (4.1) where u is a function of two independent variables x and t and c denotes a positive constant. The variable x is commonly identified with "position" and t with "time"; c is a given positive constant. Physically u can represent the normal displacement of the particles of a vibrating string. Here the characteristics are the two families of lines x ± ct = constant in the xtplane. Introducing them as coordinates by putting (4.2) x+ ct=~, x-ct=1J, (4.1) becomes (4.3) u~=O. Assume that the domain of u, as a function of x, t or, equivalently, as a function of ~,1J is convex. Since (u~)." = 0 it follows that u~ is independent of 1J, say, ul;.= J'm, and then u= Jf'm~+ G(1J). That is, u=F(~)+ G{1J). (4.4) In the original variables we find that u is of the form (4.5) Here u E C 2 if and only if F, G, E C 2• Thus the general solution of (4.1) is obtained by superposition of a solution F(x+ct)=v of vt-cvx=O and of a solution G(x-ct)=w of wt+cwx=O. This corresponds to the fact that the differential operator u=F(x+ct)+ G(x-ct). (4.6) can be decomposed into L= (i._ at c~)(i.+ c~). ax at ax (4.7) Thus the graph of u(x, t) in the xu-plane consists of two waves propagating without change of shape with velocity c in opposite directions along the x-axis. (See p. 5.) 38 4 The One-Dimensional Wave Equation We impose the initial conditions ut(x,O)=g(x). (4.8) For u of the form (4.5), we have at t=O u(x,O)= F(x) + G(x) = f(x), ut(x, O) = CF'(X) - cG'(x) = g(x). (4.9) (4.10) u(x,O)=f(x), Differentiating (4.9) with respect to x and solving the two linear equations for F' and G we obtain I F'(x) Cf'(X)+g(x) 2c or, F(x)=f~) + G'(x)= cj'(x)- g(x) 2c ;c foxg(~)d~+8, (4.11) (4.12) G(x)=f(x) __ I rxg(~)d~+e, 2 2c)0 with suitable constants 8, e. Here 8 + e = 0 by (4.9). Hence u(x,t) = F(x+ ct) + G(x- ct) I =-2I (J(x + ct) + f(x - ct)) +-2 c f x + ct x-ct g(~)d~. (4.13) For f E C 2 and gEe 1 this actually represents a solution u E C 2 of the initial-value problem (4.1), (4.8). We see from (4.13) that u(x,t) is determined uniquely by the values of the initial functionsJ,g in the interval (x, -ct,x+ct) of the x-axis whose end points are cut out by the characteristics through the point (x,t). This interval represents the domain of dependence for the solution at the point (x, t) as shown in Figure 2.2. ---r----------~--------------------~--------x o x - ct x + ct Figure 2.2 39 4 The One-Dimensional Wave Equation --~------------~----~--------~-------------x o x -ct x + ct Figure 2.3 Conversely, the initial values at a point (~,O) of the x-axis influence u(x,t) at points (x,t) in the wedge-shaped region bounded by the characteristics through (~, 0), i.e., for ~ - ct < x < ~ + ct. This indicates that for our equation "disturbances" or "signals" only travel with speed c as shown in Figure 2.3. We saw that formula (4.5) represents a solution uEC 2(1Ji 2) of (4.1) for any j,g, E C 2(1Ji). One is tempted to consider any u of the form (4.5) for "general" j,g, as a generalized or weak solution of (4.1) even though u may not have derivatives in the ordinary sense. One easily verifies that any function u of the form (4.5) satisfies the functional equation u(x,t) - u(x + cr,t+ r) - u(x- CT/,t+ 11) + u(x+ Cr-CT/,I+ r+11)=O. (4.14) Geometrically, for any parallelogram ABCD in the xl-plane bounded by four characteristic lines, (see Figure 2.4), the sums of the values of u in opposite vertices are equal, that is, u(A)+u(C)=u(B)+ u(D). (4.15) Every solution of (4.1) is of the form (4.5) with F, G, E C 2 and thus satisfies (4.14). Conversely, using Taylor expansions for small r,11, every C 2-solution of (4.14) satisfies (4.1). Thus (4.14) can be viewed as a weak formulation of equation (4.1). We use (4.4) to solve an "initial-boundary-value" problem for (4.1). Assume the wave equation to be satisfied only in a fixed x-interval 0< x < L for all I> O. Then we can prescribe, in addition to the initial data u=j(x), 40 ut=g(x) forO<x<L, t=O (4.16) 2 Second-order equations A D B c --~------------------------------------x o Figure 2.4 certain "boundary" conditions, for example u=a(t) forx=O O<t, u=/3(t) forx=L O<t. We are interested in the solution of (4.1) in the strip (4.17a) (4.17b) (4.18) O<x<L, O<t. We divide the strip into a number of regions by the characteristics through the comers and through the points of intersections of the characteristics with the boundaries, etc. as shown in Figure 2.5. In region I the solution u is determined by the formula (4.13) from the initial data alone. In a point A = (x, t) of region II we form the characteristic parallelogram with vertices A, B, C, D and get u(A) from (4.14) as u(A)=-u(C)+u(B)+u(D), (4.19) with u(B) known from boundary condition (4.17a) and u(C),u(D) known since C,D lie in I. Similarly, we get u successively in all points of the regions III, IV, V, .... If we want the solution u of this "mixed" problem to be regular (e.g., to be of class C 2 ) in the closure of the strip, the data f,g, a, /3 have to fit together in the comers so that u and its first and second derivatives come out to be the same when computed either from f,g or from a,/3. We clearly need the compatibility conditions, a (0) = f(O), a'(O) = g(O), a"(O) = c2j"(O) /3(0)= f(L), /3'(0) = g(L), /3"(0) = c2j"(L). (4.20) 41 2 Second-order equations u =a(x) o u u = f(x), Ut = (3(x) x = g(x) Figure 2.5 These actually are also sufficient for uEC 2 whenj,a,/3 EC 2 and gEC l • For example, for A EI and u(A) given by (4.19) we take the limit as A~D for D fixed. Then u(B)~a(O), u(C)~j(O) and u(A)~- j(O) + u(D)+a(O) = u(D), if (4.20) holds. If, instead, a(O):;6f(O), we would find that u has a jump all along the line x = ct. An alternative method ("separation of variables") gives the solution at one stroke by expansion into eigenfunctions. For simplicity, take the case where L = 'IT and a = /3 = 0 in (4.11), so that we have homogeneous boundary conditions. Then, for each t, u(x,t) can be expanded into a Fourier sine series 00 u = ~ an (t)sinnx. (4.21) n=l Substituting into (4.1) we find that ait) satisfies the ordinary differential equation + n 2c 2an = 0, hence that an is of the form a:: an(t) = Cn cos(nct) + dnsin(nct). (4.22) Here the constants cn,dn can be found from the initial conditions (4.16) which require that 00 j(x)= ~ cnsinnx, n-l 42 00 g(x) = c ~ ndnsinnx, n-l (4.23) 4 The One-Dimensional Wave Equation so that by Fourier en=~ ('lTf(x)sinnxdx, dn =2en'fT 'fT )0 i'ITg(x)sinnxdx. 0 (4.24) In applications we usually deal only with a bounded domain for our solutions, and are led to initial-boundary-value problems rather than to "pure" initial-value problems. An example is the normal displacement u(x,l) of a vibrating string of length 'fT. Then u satisfies the boundary conditions u(x,O)=u(x,'fT)=O, if the ends of the string are held fixed, and initial conditions of type (4.16) if the initial normal' displacement and normal velocity of each particle of the string are prescribed. PROBLEMS 1. Let j(x),g(x) have compact support (i.e., vanish for all sufficiently large Ixl). Show that the solution u(x,t) of (4.1), (4.8) has compact support in x for each fixed t. Show that the functions F, G in the decomposition (4.5) for U can be of compact support only when f~oog(€)~=O. 2. Let a be a constant =1= -c. Find the solution u(x,t) of (4.1) in the quadrant x>O,t>O, for which u=j(x), ut=g(x) for t=O, x>O ut=aux for x=O, t>O, wherejandg are of class C 2 for x>O and vanish near x=O. (Hint: Use (4.5». Show that generally no solution exists when a = - c. 3. Solve the initial-boundary-value problem ("mixed problem") Utt=Uxx forO<x<'1T, 0< t, u=O for x=O,'1T; 0< t, u=l, ut=O forO<x<'1T,t=O, by (a) piecing together, using (4.14), and (b) Fourier series. Check that the solutions agree. 4. Let the operators LI'~ be defined by L1u=aux+buy+cu, ~u=dux+~+ ju, where a,h,c,d,e,j are constants with ac- hd=l=O. Prove that (a) the equations L1u= WI> ~u= W2 have a common solution u, if L1W2= ~~I' (Hint: By linear transformation reduce to the case a = e = I, h = d = 0.) (b) The general solution of LI~u=O has the form U=UI+u2, where L1UI=0, L 2U2=0. 5. Solve Utt - c2uxx = x 2 for 0 < t u=x, and all x ut=O for t=O. (Hint: First find a special time independent solution of the P.D.E.) 6. Find a solution of 43 2 Second-order equations (A constant) of the form u=f(x 2 -c2t1=f(s), when f(O) = I, in form of a power series in s. 7. With L defined by (4.1) prove that (a) Lu=O, Lv=O implies L(utvt + cluxvx ) =0, (b) Prove thatfor Lu=O, Lv=O for a< x<b, 1>0 and u=O for x=a,b; 1>0. d (bl dl J~ 2 (utVt + cluxvx)dx =0. a 8. For the solution (4.21), (4.22) of the wave equation express the "energy" ('IT I Jo 2 2 2(ut +ux)dx, in terms of cn' dn• 9. Find the Fourier series solution (4.21) for the case u(x,O)=i-li-xj. Ur(x,O)=O forO<x<'IT, (vibration of string plucked at center) and calculate its energy. 10. Find in closed form the solution u(x, I) of Lu=utt-cluxx=O for O<X, 0< I, u(O,/)=h(/) for 0<1, u(x,O)=f(x) ut(x,O)=g(x) forO<x, withf,g,h E C 2 for nonnegative arguments and satisfying h(O)=f(O), h'(O) = g(O), h"(O) = c2j"(O). Verify that the u obtained has continuous second derivatives even on the characteristic line x = cl. 5. Systems of First-order Equations It is convenient to treat general second-order equations as part of a still more general theory, that of first-order systems, to which in principle all higher-order single equations can be reduced. Thus the linear equation (3.1) for u(x,y) is reduced to a first-order system by introducing the new dependent variables (5.1) yielding the equations (5.2) (5.3) 44 5 Systems of First-order Equations (Courant-Lax Theory) More generally, writing t for y, we consider an N-vector (column vector) u{}U(X,t), satisfying an equation au A(x,t)ai+B(x,t) au ax = C(x,t)u+D(x,t), (S.4) (S.5) for given square matrices A,B,C of order N and column vector D. The Cauchy problem for (5.5) prescribes the value of u on a curve t=<t>{x) in the xt-plane (S.6) u= u(x,cp(x» = j(x). The curve is characteristic if we cannot find the derivatives of u from the data on the curve. Now (5.5), (5.6) imply on t=<t>{x) that (S.7) Aut+Bux = Cj+D, or (5.8) (A -cp' B )ut = Cj+ Dd- BJ'. Thus, characteristic curves are those for which the matrix A - cp' B is singular, or for which the Nth-degree differential equation det(Adx-Bdt)=O (S.9) holds. For the initial-value problem to be treated here we prescribe the values of u on the x-axis, assumed to be non-characteristic: (S.lO) u(x,O)= j(x), (S.11) detA *0 for t=O. For small t we can then solve for Ut in (5.5) getting a new equation ut+B(x,t)ux=Cu+D (S.12) (With new matrices B, C and vector D.) The characteristic differential equation (5.9) now takes the form det( ~~ / - B ) =0 (5.13). (/ = unit matrix) which factors into conditions of the form dx dt =Ak(X,t), (S.14) where ~(x,t) denotes the kth eigenvalue of the matrix B(x,t). We assume these eigenvalues to be real, so that for each k (S.14) is satisfied by a one-parameter family of characteristic curves Ck • More precisely, we assume the system (S.5) to be hyperbolic in the sense 45 2 Second-order equations that there exists a complete set of real eigenvectors ~ 1, ••• , ~N of B such that Be = Ake, (5.15) where the ~k are linearly independent and depend "regularly" on x and t. (This certainly holds where the eigenvalues of B are real and distinct.) The column vectors then form the columns of a nondegenerate matrix f=f(x,t) for which e (5.16) Bf=fA, where A is the diagonal matrix whose diagonal elements are the eigenvalues Ak • Introducing a new unknown vector v by u = fv, we find from (5.12) that v satisfies (5.17) with new coefficients c=f-1Cf-f-1ft -f-1Bfx' and initial conditions for t=O. (5.18) We have reduced (5.5) to "canonical form" where A =1 and B is diagonal. If v has components Vi' c = (Cik ), and d has components di we find from (5.17), along a characteristic Ci of the ith family, v=f-Y=g(x) dVi = dt aVi + dx aVi = aVi +\ aVi = L C-kVk+d.. at dt ax at ax k I (5.19) I The ith backward characteristic Ci through a point (X, T) has an equation (5.20) (obtained by solving the ordinary differential equation (5.14)). Then by (5.18), (5.19), integrating along Ci (see Figure 2.6) vi(X, T) = gi (ai (0, X, T» + [T( ~ CikVk + d; )dt, (5.21) where in the integrand x has to be replaced by a;(t, X, T). Formula (5.21) resembles a system of integral equations except that the domain of integration is different for each component of v. We write (5.21) symbolically as v= W+Sv, (5.22) where W is the vector (considered known) with components, W;(X, T) = gi(ai(O,X, T» +loTdi(ai(t,X, T),t)dt (5.23) and S is the linear operator taking a vector v with components vk(x,t) into 46 5 Systems of First-order Equations (Courant-Lax Theory) (X, T) __ ~~ ____L -__- L______ ~ ______ ~ ______L -_____ x Figure 2.6 a vector w = Sv with components w;(X, T) = r ~ C;k( a;(t,X, T),t)Vk( a;(t,X, T),i)dt. T )0 k (5.24) Given sufficient regularity of our data, the mapping S: C~C is continuous in the space C of continuous bounded vectors v(x,t) with domain in the strip 0 ~ t ~ T, using in C the "maximum norm": Ilvll = sup k=l, ... ,N IVk(X,t)l· (5.25) x;O<I<'T The norm IISII of the operator S (the supremum of IISvll for Ilvll = 1) obviously is bounded * by the constant q=T sup ~ IC;k(X,t)l. i,x k O<I<'T (5.26) For q < 1, i.e., for T sufficiently small, the mapping S is contractive. Then (5.22) has a unique solution vEe obtainable by the process of iteration (5.27) (Convergence follows by comparison with a geometric series.) The resulting v will satisfy the "integral equations" (5.21), but it is not certain that these imply the differential equations (5.19) or (5.17) until we have established existence of continuous partial derivatives for v. For that purpose we shall work in the narrower Banach space C 1 of vectors vex, t) for which v and Vx are continuous and bounded for 0 ~ t ~ T and all x, in which we choose as norm (5.28) IlIvlll =max(lIvll, Ilvxll)· ·We assume, for convenience, that the C;k(X,t) and their first derivatives are bounded uniformly for - 00 < x < 00, 0.;; t.;; T. 47 2 Second-order equations The restriction of S to C 1 maps C 1 into itself and has its norm for C 1 bounded by q*= '1"( ~ (!~~ lcilcx(x,/)1 + Icjk(x,/)I) t~~;)ajx(/,X, T)I) +'1" ~ SUpICjk(X,/)I. k (5.29) x,t For q* < I equation (5.22) has a solution in C I, provided WE C I. Obviously Sv for v E C ~ can be differentiated with respect to T as well. Thus, convergence of the v n and v: implies convergence of vtn • Hence in the limit we obtain a solution v of the original initial-value problem for our partial differential equations. The condition q* < I will again be satisfied for '1" sufficiently small. In this way, we obtain an existence theorem for a sufficiently small I-interval. Here v can be continued as long as our ordinary differential equations for the characteristics lead to sufficiently regular solutions permitting us to define functions a;(/,X, T) describing characteristics from (X, T) backwards to the x-axis. Further extensions to quasi-linear systems were given by Courant and Lax. We have solved the pure initial-value problem in the linear case, assuming that the initial data are known on the whole x-axis. The method described extends to mixed initial-boundary-value problems as well. For simplicity take as domain for the vector v the first quadrant x > 0, I> O. We then need, in addition to initial conditions, v=g(x) for O<x, 1=0, (5.30) boundary conditions on the half line x = 0, 0 < I. The number of these conditions depends on the number of positive eigenvalues Ak of the matrix B. Let, say, the number r be such that (5.31) The characteristics Cj of the ith family then have positive slopes for i=I, ... ,r, negative ones for i=r+I, ... ,N. A backward characteristic X=a;(/,X,T) (5.32) through a point (X, T) with 0 < X, 0 < T for i = r + I, ... , N will hit the positive x-axis in a point Pj(X,T). For i=I, ... ,r, it will either hit the positive X-axis or positive t-axis in a point, again denoted by P;(X, T). On the positive I-axis we prescribe the values of r linear combinations of the components of v, which we assume to have been brought into the form n Vj- ~ k=r+1 Yjk(t)Vk=hj(t) for 0< I, x=O;i= 1, ... ,r. (5.33) We redefine the operator S acting on vectors v. Let, for a vector v(x,/), the component Wj(X, T) of W= Sv be defined by (5.24) if Pj(X, T) lies on the 48 5 Systems of First-order Equations (Courant-Lax Theory) x-axis, in particular, whenever i=r+ 1•... ,N. If, on the other hand, P;(X, T) lies on the t-axis, say P; = (0, to), we take N N w;(X, T)= ~ 'Y;k(tO) Lto ~ cks(ak(t,O,to),t)v.. (ak(t,O,to),t)dt k-r+l N +~ k= 1 0 s=r+l fto c;k(a;(t,X,T),t)vk(a;(t,X,T),t)dt. T (5.34) (Here the second sum corresponds to the expression for v;(X, T) in terms of v;(P;) and integrals along C;, the first sum corresponds to v;(P;) expressed by the Vk(P;) for k> r, which, in turn, are expressed by integrals over backward characteristics through P; [See Figure 2.7].) We again get a set of equations formally describable by (5.22) with a known W, which can be solved for 0 <:; t < 'T, with 'T sufficiently small. Solutions of problems in a finite interval 0 <:; x <:; L can be reduced to pure initial-value problems, and to problems of the type just discussed, by breaking up the domain 0", x <:; L, 0 < t <:; 'T into suitable portions by characteristics, as was done earlier for the one-dimensional wave equation. The number of boundary conditions on x = 0 equals the number of positive Ak , that on x = L equals the number of negative Ak • (X. T) Figure 2.7 49 2 Second-order equations PROBLEM Write IItt=c'luxx , u(x,O)=f(x), ut(x,O)=g(x) as an initial-value problem for the vector (Ul,U2) = (IIt,Ux )' Reduce the system to the canonical form (5.17) and solve the problem. 6. A Quasi-linear System and Simple Waves Consider a quasi-linear system of equations for functions v1(x, t), ... , vN(x,y) forming a column vector v(x,t), of the special form vt+B(v)vx=O (6.1) with a square matrix B(v) depending on the dependent variables. We assume that (6.1) is hyperbolic in the sense that B(v) has real distinct eigenvalues for all v in question. The general solution v(x, t) can be visualized as forming a two-dimensional surface in N-dimensional v-space, referred to the two parameters x,t. Special explicit solutions can be obtained by requiring that this surface degenerates into a curve, that is, that the range of the solution v is one-dimensional. Such v can be represented in the form (6.2) v=F(O), where the scalar 0 is a function of x and t. Substituting into (6.1) yields F'(O)Ot+B(F)F'(O)Ox=O. (6.3) Thus F'(O) must be an eigenvector of the matrix B(F) belonging to an eigenvalue A such that Ot + AOx = O. These conditions can be satisfied by thinking of B(v) as constituting a field of matrices in lV-dimensional v-space. With each point v we associate an eigenvector V = V( v) and corresponding eigenvalue A=A(V), varying smoothly with v. We take a vector F= F(O) correspond.ng to a particular solution of the system of ordinary differential equations dF (6.4) dO = V(F). Along this solution the eigenvalue A(V)=A(F(O» becomes a known function c(O). Taking for O=O(x,t) any solution of the scalar equation °t+c(O)Ox=O (6.5) we have in v=F(O(x,t» a solution of (6.1) called a simple wave. The solution of (6.5) with initial values O=</>(x) for t=O is given by the implicit equation [See Chapter I, (6.28)]. o=</>(x- c(O )t). 50 (6.6) 6 A Quasi-linear System and Simple Waves PROBLEM Solve u//-(1 + Ux )2Uxx =0 with initial conditions (containing an arbitrary function h) u=h(x), u,= -h'(x)-th,2(x) for t=O. (Hint: Convert to a system for the vector v with components [Answer: VI = Ilx, V2 = u/.) u=h(x-(1 +9 )t)+Ih,2(x-(1 +9 )t), with 9(x,t) given implicitly by 9=h'(x-(1 +9)t).] Find the domain of existence of u when h(X)=X2. 51 3 Characteristic manifolds and the Cauchy problem* 1. Notation of Laurent Schwartzt This multi-index notation is extremely convenient for partial differential equations, keeping us from drowning in a flood of subscripts. We consider here "vectors" ~ = (~]' ... ,~) with n (usually) real components and "multiindices" a=(a], ... ,a,,) which are vectors whose components are nonnegative integers. With a multi-index a we associate the scalars a! =a]!a2!' .. a,,!. lal=a] +a2+··· +an , From a vector ~ (Ll) and multi-index a we form the monomial ~a = ~1.~22 ... ~n"". (1.2) By Ca we generally denote a coefficient depending on n nonnegative integers a], •.. ,a,,: Ca = Ca •... ..". The general mth-degree polynomial in n variables form P(~) = ~ lal<m Ca~a. (1.3) ~], ... '~n is then of the (1.4) Using the Cauchy differentiation symbol Dk = a/aXk' we introduce the "gradient vector" D =(D], ... ,Dn ), and define the gradient of a function u( X], ••• , xn) as the vector (1.5) *([7D t([12], [15D 52 1 Notation of Laurent Schwartz The general partial differentiation operator of order m is then am (1.6) where /a/=m. For a function f( x) = f(x!, ... , x n ) we have the formal power series expansion f(x+y)= L J,(D'1(x))ya. a. a (1.7) We callf(x) real analytic in a region 0 of Rn if for each xEO the series on the right of (1.7) converges absolutely and represents f( x +y) for all sufficiently small vectors y. We call f( x) real analytic at a point XO if f( x) is defined and real analytic in a neighborhood of XO in Rn. It is clear that a functionf(x) which is real analytic at the origin of Rn can be extended by its power series to complex x as a function with continuous derivatives of all orders in a neighborhood of the origin in complex n-space en. Conversely let f(x) be defined and continuous in a complex neighborhood of the origin and let the first derivatives of f exist and be continuous in that complex neighborhood. Thenf(x) is real analytic in a neighborhood of the origin of Rn. Indeed by repeating the ordinary Cauchy formula for functions of one complex variable, we derive for f near 0 in Rn the multiple integral representation where the paths of integration are circles of sufficiently small radius about the origin in the complex plane. Expanding the integrands one sees immediately that f(x) is represented by a convergent power series for all sufficiently small /xk /. The most conspicuous property of real analytic functionsf(x) is that of unique continuation: Iffis real analytic in an open connected set 0 C Rn, then f is already determined uniquely everywhere in o by its values in an arbitrarily small neighborhood of some point of O. PROBLEMS Let x,y denote a vector and a,{3 multi-indices with n components. Prove the following identities: 1. the binomial theorem (1.9) 53 3 Characteristic manifolds and the Cauchy problem 2. Leibnitz's rule for scalar functionsf(x),g(x) L Da(Jg)= f> p,y a~!, (DPj)(DYg) f' .y. (1.10) f3+y='a 3. geometric series: for IXkl < 1 for k= l, ... ,n ~ x a = -=-_--.,---l--;-::--~ (l-x\) ... (l-xn ) a (1.11 ) 4. for a nonnegative integer m (1.12) (1.13) 2. The Cauchy Problem* In the Schwartz notation the general mth-order linear differential equation for a function u(x)=u(x\, ... ,xn) takes the simple form Lu= L lal<m Aa(x)D"u= B(x). (2.1) The same formula describes the general mth-order system of N differential equations in N unknowns if we interpret u and B as column vectors with N components and the Aa as N X N square matrices. Similarly the general mth-order quasi-linear equation (respectively system of such equations) is Lu= L lal=m AaDau+ C=O, (2.2) where now the A and C are functions of the independent variables Xk and of the derivatives D f3u of the unknown u of orders IPI..; m - 1. More general nonlinear equations or systems F(x,Dau) =0 (2.3) can be reduced formally to quasi-linear ones by applying a first-order differential operator to (2.3). On the other hand, an mth-order quasi-linear system (2.2) can be reduced to a (larger) first-order one, by introducing all derivatives Df3u with IPI..; m-l as new dependent variables, and making use of suitable compatibility conditions for the Df3u. The Cauchy Problem consists of finding a solution u of (2.2) or (2.1) having prescribed Cauchy data on a hyper-surface S C IRn given by l/>(x\, ... ,xn)=O. * ([23D 54 (2.4) 2 The Cauchy Problem Here cp shall have m continuous derivatives and the surface should be regular in the sense that (2.5) The Cauchy data on S for an mth-order equation consist of the derivatives of u of orders less than or equal to m - 1. They cannot be given arbitrarily but have to satisfy the compatibility conditions valid on S for all functions regular near S (instead normal derivatives of order less than m can be given independently from each other). We are to find a solution u near S which has these Cauchy data on S. We call S noncharacteristic if we can get all Dfiu for lal = m on S from the linear algebraic system of equations consisting of the compatibility conditions for the data and the partial differential equation (2.2) taken on S. We call S characteristic if at each point x of S the surface S is not noncharacteristic. Characteristic surfaces naturally occur in connection with singular solutions of a certain type. If u is a (generalized) solution of (2.1) of class C m - l which has jump discontinuities in its mth-order derivatives along a surface S, then S must be a characteristic surface. (See Chapter 2, p.34.) To get an algebraic criterion for characteristic surfaces we first consider the special case where the hyper-surface S is the coordinate plane Xn = O. The Cauchy data then consist of the Dfiu with 1,81 < m taken for t=O. Singling out the "normal" derivatives on S of orders .s; : m - 1: D:U=o/k(X1,,,,,Xn_ l ) for k=O, ... ,m-l and xn=O (2.6) we have on S DfiU=Df'Df2 ... D:~-Nfi" (2.7) provided that ,8n < m. In particular for I,81.s;;: m - 1 we have here the compatibility conditions expressing all Cauchy data in terms of normal derivatives on S. Let a* denote the multi-index a*=(O, ... ,O,m). (2.8) In the differential equation (2.1) or (2.2) taken on S it is only the term with %, ... ,o/m-l and hence in" terms of the Cauchy data. All others contain derivatives D"u with lanl.s;;: m - 1. Thus Da*u, and hence all D"u with lal.s;;: m, are determined uniquely on S, if we can solve the differential equation for the term D a*u. This is always possible in a unique way if and only if the matrix A a * is nondegenerate, i.e., det(Aa*)~O. For a single scalar differential equation this condition reduces to Aa*~O. In the linear case the validity of the condition a = a* that is not expressible by (2.7) in terms of (2.9) does not depend on the Cauchy data on S; in the quasi-linear case, however, where the Aa depend on the Dfiu with I,81.s;;: m-l and on x, one has to know the o/k in order to decide if S is noncharacteristic. 55 3 Characteristic manifolds and the Cauchy problem Condition (2.9) involves coefficients of mth-order derivatives. We define the principal part Lpr of L (both in (2.2) and (2.1» as consisting of the highest order terms of L: (2.10) Lpr= ~ AQDQ. IQI-m The "symbol" of this differential operator is the matrix form ("characteristic matrix" of L): A(O= ~ AQr a • (2.11) lal=m Here the N x N matrix A(n has elements that are mth-degree forms in the components of the vector r = (r \, ... ,rn). In particular, the multiplier of D; in Lpr is Aa*=A("1), where "1=(O, ... ,O,I)=Dcp. (2.12) is the unit normal to the surface cp = xn = 0. The condition for the plane cp = xn = to be noncharacteristic is then Q(Dcp) *0, (2.13) where Q = Q(n is the characteristic form defined by (2.14) Q(r)= det(A(r» for any vector r. (In the case of a scalar equation (N = 1) the characteristic form Q(n coincides with the polynomial A(r).) We shall see that quite generally (2.13) is the condition for a surface cp=O to be noncharacteristic. Take now a general S described by (2.4). By assumption (2.5) the first derivatives of cp do not vanish simultaneously. Suppose that in a neighborhood of a given point of S, the condition CPxn *0 holds. The transformation ° y.= I { Xi cp(x\, ... ,xn ) fori=I, ... ,n-1 for i= n (2.15) is then locally regular and invertible. By the chain rule, au "" aXi au = ~ Cik aYk ' (2.16) where the (2.17) are functions of X or of y. Denoting by C the matrix of the Cik and introducing the gradient operator d with respect to y with components a di=-a ' ~i (2.18) we can write (2.16) symbolically, as D=Cd, 56 (2.19) 2 The Cauchy Problem taking D and d to be column vectors. Generally, then for lal = m Da={Cdr+Ra, (2.20) where Ra is a linear differential operator involving only derivatives of orders "m - 1, (arising from the dependence of C on x) and (Cd)a is formed as if C were a constant matrix, i.e., not applying differentiations to the elements of C. Then the principal part of the operator L in (2.2) or (2.1) transformed to y-coordinates is given by Lpr= ~ AaCCdr=tpr lal=m (2.21) and its symbol, the characteristic matrix of t, by A{7J)= ~ Aa{C7Jr· lal=m (2.22) For the regular mapping (2.15) x-derivatives of orders less than or equal to r are linear combinations of y-derivatives of orders less than or equal to r, and conversely. Hence noncharacteristic behavior of S is preserved under the transformation. Thus S is noncharacteristic for L if the plane y n = 0 is noncharacteristic with respect to the operator L transformed to y-coordinates, i.e., if det{A{7J))=det( ~ lal=m AaCC'l/r)=Fo, (2.23) for the column vector 7J with components (0, ... ,0, 1). But then S= C7J is just the column vector with components aYn/ih; = D;q" that is, the vector Dq,. Thus, the condition for noncharacteristic behavior of S can again be written as (2.13). If u in (2.2) stands for a vector with N components, the condition for S to be a characteristic surface Q{Dq,)=det( ~ lal=m Aa{Dq,r)=o (2.24) signifies the vanishing on S of a form of degree Nm in the components of Dq,. In the linear case (where the coefficients of that form only depend on x and not on u) we can consider a one-parameter family q,(Xl""'Xn)= const. = c of characteristic surfaces. Then (2.24) becomes a first-order partial differential equation of q" homogeneous of degree Nm in the first derivatives of q, from which q, can be determined by the methods of solution for single first-order equations. For example in the case of a linear first-order system n Lu= ~ A;{x) a a~; +B{x)u=w{x), (2.25) (u and w being N-vectors and the A; and B, N X N matrices) the condition 57 3 Characteristic manifolds and the Cauchy problem for a characteristic surface is det( ~ ~<t> Ai) =0. i= I uXi (2.26) Alternately a single characteristic surface S gives rise to a partial differential equation, when described by an explicit equation <t>(x l , ... ,Xn) = Xn - tf;(x l ,. ",Xn-I) =0. (2.27) Equation (2.24) in the linear case becomes a first-order partial differential equation for the function tf;. Take, e.g., the wave equation (2.28a) for u= U(XI,X2,t). A characteristic surface t=tf;(xI,x0 then satisfies the equation 1 = c2( tf;;. + tf;;,) (2.28b) already encountered in Chapter 1, p. 26. Thus equation (2.28b) regulates the propagation of singularities for equation (2.28a). The characteristic form Q(n of the operator L defined by (2.14), (2.11) generally depends on and on the arguments of the Aa, that is, on x and the DPu with IPI..;; m - 1. A hyperSurface is characteristic for the operator L (and in the nonlinear case for given Cauchy data Dfiu) if Q(n=O for the normal vector r of the surface. We call L elliptic if Q(n,,=O for all real r,,= o. In that case there exist no real characteristic hypersurfaces. In the case of an operator L with real coefficients, ellipticity of L is then equivalent to definiteness of the form Q(r) (at least for n> 1): the form Q(n is of constant sign for r,,=O. This, of course, can only happen when the degree mN of Q is even. The standard example for an elliptic L is the + ... + for which Laplace operator !J. = r Dr D; n Q(r)= ~ r/ i= I is positive definite. The extension of the notion of "hyperbolicity" to general quasi-linear systems is more complicated. We can define characteristic manifolds for more general nonlinear equations as well. Take, for example, an mth-order scalar equation for a function u=u(xl, ... ,xn), which we write in the form (2.29a) where Pa = Dau for lui..;; m. Suppose that on the hypersurface S given by (2.4) we have <t>x. ,,=0. Differentiating (2.29a) with respect to Xn we obtain the equation dF "'" dF 0=1)+ ~ 1) Dn Dau . r Xn a 'Pa (2.29b) Since rn"=O for = D<t>, the condition for S to be characteristic with respect 58 3 Cauchy-Kowalewski Theorem to (2.29b) is simply ~ ~F (D4>t =0. I~m 'Pa (2.30) We use (2.30) to define what is meant by S to be characteristic with respect to (2.29a). Observe that this condition generally involves not only the Cauchy data but all derivatives of u of orders ~ m on S. In the example of the first-order equation (7.1) of Chapter 1, condition (2.30) for a characteristic (projection) 4>( x,y) = const. would read F;,4>x + Fq4>y = O. Since here 4>x dx + cf>y dy = 0 along S, the condition is equivalent to the second equation in (7.10) of Chapter 1. PROBLEMS 1. Identify the special cases of "characteristic curves" in Chapter 2 (1.12) and (5.13) with the general formula (2.13). 2. Let u(X)=U(Xb""Xn ) and its derivatives of orders <m vanish on the hypersurface S given by (2.4). Show that on S D"u=JL(DCPr for JaJ=m, (2.31) where the factor of proportionality JL depends on u but not on a. Show that in particular for u of the form u=cpmv(x) with vEC m D"u=m!(DCPrv. (Hint: Transform S by (2.15) into the planeYn=O.) (2.32) 3. Cauchy-Kowalewski Theorem This theorem concerns the existence of a solution of the Cauchy problem formulated earlier for the case of analytic data and analytic equations. We restrict ourselves to quasi-linear systems of type (2.1), since more general nonlinear systems can be reduced to quasi-linear ones by differentiation. We assume that the initial surface S is analytic in a neighborhood of one of its points xo, that is near Xo the surface S is given by an equation 4>(x)=O, where 4> is real analytic at xo, (that is, given by a convergent power series in x - xo) and that D4>=I=O at xo, say, Dn4>=I=O. On S we prescribe compatible Cauchy data DPu for 1,8l ~ m - 1 which shall be real analytic at x-xo (e.g., represented by power series in (XI-X?, ... ,Xn_lx~ The coefficients Aa and B shall be real analytic functions of their arguments x and DPu at xo, that is, given by convergent power series in x-xo and in (DPu-DPu~ in a neighborhood of xo, where DPuo is the value of DP corresponding to the Cauchy data at xO. Let, moreover, S be noncharacteristic at Xo (and hence in a neighborhood of x~ in the sense that Q(D4»=I=O. Then the Cauchy-Kowalewski theorem asserts that there -I»' 59 3 Characteristic manifolds and the Cauchy problem exists a solution of the Cauchy problem which is analytic at XO (given by a power series in x - xC) and that there is no other analytic solution. The proof of this general theorem consists of showing that all coefficients for a prospective power series solution u at XO can be obtained by successive differentiation from the differential equation and Cauchy data, and that the resulting series actually converges to a solution. The proof becomes easier if we reduce the problem before constructing the power series. First of all, one transforms S locally by an analytic transformation into a neighborhood of the origin in the plane Xn = O. Then by introducing derivatives of orders less than or equal to m - I as new dependent variables one reduces the system to one of the first order. We make use of the fact here that the set of real analytic functions is closed under differentiation and composition. One arrives at a first-order system in which the coefficient matrix of the term with aujaxn is nondegenerate because S is noncharacteristic. Hence one can solve for aujdxn, obtaining a system in the standard form n-I au ~ ~= ~ j=1 uXn au Aj(x,u)""il+ B(x,u), uXj (3.1) where the Aj(x,u) are square matrices (aijk) and B(x,u) a column vector with components bj' analytic in their arguments. Written out componentwise, (3.1) becomes a system for the N components t4.i of u: n-I N L aijk(x,u)DjUk+ bj(x,u). i= 1 k= 1 Dnt4.i= ~ (3.2) On xn=O, near 0, we have prescribed initial values u=f(x). Here we can assume that f = 0, introducing u - f as the new unknown function. Thus, is the initial condition for (3.1) or (3.2). By assumption the aijk and bj are given by convergent power series in the xp Ur near x = u = O. Once all derivatives of u(x) at x=O have been determined, u, if analytic, is determined uniquely and given by the Taylor series. Now this determination is carried out easily from (3.2) and (3.3). Indeed (3.2) permits us to express successively all derivatives Dau in terms of derivatives DfJu with f3n=O. First, by (3.2), Dnt4.i is expressed in terms of x,u,Dju with i=t=n; then also DYDnu, for Yn =0, by applying DYu to (3.2). Next, differentiating (3.2) with respect to x n' we find D;u in terms of x, u, Dju,Dnu,DjDkU,DjDnu, with i,k=t=n, and thus in terms of x,u,Dju,DjDku and then also DYDn2u for Yn=O. Continuing in this way we find an expression for any D~ in terms of x,u,DfJu with f3n=O. More precisely, this expression will be a polynomial in the DfJu and in derivatives of the aijk(x,u) and /J.i(x,u) with respect to the Xj and Ur with coefficients which are nonnegative integers. Putting then x=O, all DfJu with f3n=O vanish and 60 3 Cauchy-Kowalewski Theorem we find that at the origin, D~m = Pa,m(DY8paijk,DY8pbj)' (3.4) where DY indicates differentiation with respect to x and 813 with respect to u, all derivatives taken at the origin, and Pa,m is a polynomial with nonnegative coefficients. One sees this more clearly from the model of the ordinary differential equation u'=b(x,u) for a scalar function u(x) of the scalar variable x with initial condition u(O) = O. One finds successively for x = 0, u=O, u'=b, etc. Clearly an analytic solution u(x), if it exists, is given by uj = L l,(D~j)xa, a. a (3.5) with Dauj obtained from (3.4). It remains to show that the formal series converges for Ixl sufficiently small and that it actually represents a solution of (3.2), (3.3). Convergence in (3.5) depends on getting appropriate estimates for the expression (3.4) for the D~j' This is difficult because of the complicated structure of the polynomials and can be avoided by just using the positive character of the coefficients. The arguments of the PaJ are the derivatives of the aijk and bj with respect to the X k and Ur at x = u =0. These in tum differ from the coefficients of the power series for the aijk and bj in terms of x and u only by positive factors. Let us replace the differential equation (3.2) by (3.6)' with initial condition v=O for xn=O (3.6a) and assume (3.6), (3.6a) has a solution v analytic at O. Then the coefficients of its power series are determined by Davm= Pa,m( D Y8 Paijk,D Y8 Pbj). (3.7) Assume now that aijk' bj majorise aijk' bj in the sense that I( D Y8 Paijk) x=u=ol ,,( D Y8 Paijk) x=u=o' I( D Y13 Pbj )x= u=ol ,,( D Y8 Pbj) x=u=o' for all f3 and y. Then in (3.4), (3.7) Ipa,m( Dr8paijk,Dr13Pbj)I" Pa,m( D r13 paijk,D r8 Pbj) (3.8) 61 3 Characteristic manifolds and the Cauchy problem (with derivatives taken at x = u = 0). Hence, since the series ~ ~! (Davj\=ox a (3.9) converges absolutely in a neighborhood of the origin, the same holds for the series (3.6), by comparison. It is thus sufficient to find a majorising equation (3.6) for which existence of an analytic solution v satisfying the initial condition (3.6a) can be established. Consider generally a function F(x)=F(xl, ... ,xn) real analytic at x = O. Let (3.10) F(x) = ~ Caxa a for IXkl...;; r, k= 1, ... ,n. (The series will also converge for complex Xk with IXkl < r, but we shall not make use of this fact). Since the series converges for XI = ... = Xn = r we have Carla l bounded: ICal...;; Mr-Ial...;; la~! Mr- Ial . (3.11) a. for a certain M. The function G(x)= ~ C~xa, (3.12) a analytic at 0, majorises F(x) if (3.13) We write then F«G. In particular, by (Lll), (1.13), (3.11), F«~ Mr-Ialxa= a Mr n (r-x l )'" (r-xn) «~ lal! Mr-Ialxa= a a! (3.14) (3.15) Mr r-xl-x2-"'-xn Here r measures the size of the complex neighborhood IXkl <r, k= 1,2, ... ,n, of 0 in which F(x) is analytic, and M controls the magnitude of F in that complex neighborhood. Thus there exist suitable constants M,r, such that b( ) .~u« J 62 M(n-l)r2 (r - x I - ... - xn-I - u I -'"N - u )(r - x ) n . (3.16) 3 Cauchy-Kowalewski Theorem Hence we can majorise problem (3.2), (3.3) for u by one of the form D Mr2 V.=~-------------:-;-----,­ nJ (r-x,-'" where tJ = °for -xn_,-v,-'" -vN)(r-xn ) Xn = 0. The solution of this problem has the form V,=V2='" =vN = 1 N(w(s,t)-s), (3.18) where (3.19) Here the scalar w(s, t) is simply the solution of a Cauchy problem for a single first-order equation w= t Mr2(n-l) w (r-w)(r-t) s' (3.20a) (3.20b) w(s,O)=s. This problem can be solved explicitly by the methods of Chapter 1 and one verifies easily that its solution is analytic at the origin. One still has to verify that the analytic vector u constructed from (3.4), (3.5) actually satisfies (3.1). We omit the somewhat tedious but not difficult argument showing this. This then completes the proof of the CauchyKowalewski theorem. PROBLEMS 1. Solve (3.20a,b) and find a positive p such that w(s,t) is analytic for complex s,t with lsi < p, Itl < p, and hence such that the power series for w(s, t) converges for those s,t. (Answer: w=~(r+s-vr-si+4M(n-l)r210g( I-f) ). Possibly p=r/(2+32M(n-I).) 2. In the linear case the system (3.2) can be given the form n-' Dn~= ~ N ~ aijk(x)DjUk+ ~ bjk(x)Uk+Cj(X), i=' k=' k=' (3.21) It can be majorised by a system of the form Dn Vj = (r-s )~ r-t ) (M~ i,k DjVk + M~ k Vk + IL) (3.22) 63 3 Characteristic manifolds and the Cauchy problem with s,t defined as in (3.19) and with suitable constants r,M,p.. Solve (3.22) with for t-O. Show that the resulting region in which the solution u of (3.21) can be represented by a power series depends on r and M but not on p. (and hence not on the "size" of the Cj in a complex neighborhood of the origin). Vj-O 3. Let the scalar function F(x) of the scalar variable x be defined for power series 00 Ixl < I by the k F(x)=c ~ \ ' (::ik where C is a positive constant (a) Express F in integral form. (b) Prove F2«F for C sufficiently small. 4. Observe that the initial-value problem for the scalar ordinary differential equation u'=I+u2 withu(O)=O is majorised by the problem 1 v'=-- with V (0) =0. I-v Hence deduce an upper bound for the power series expansion of u(x)=tanx. 4. The Lagrange-Green Identity We recall the Gauss divergence theorem: where d / dn denotes differentiation in the direction of the exterior unit normal n ) of ag and dx-dxl ... dxn , dSx-surface element with of our region to be integration on x. We always assume the boundary sufficiently regular so that the divergence theorem applies to all u E C 1(0). The theorem can be generalized to- u E C 1(g) n CO(O) by approximating g from the interior. More generally, we have the formula for integration by parts, r-(rl .... ,r an (4.2) where u, v are column vectors belonging to C I(g) with T denoting transposition. Let now L be a linear differential operator Lu- ~ aa(x)D"u. lal<m (4.3) Let u,v be column vectors and aa be square matrices in Cm(O). Then by 64 5 The Uniqueness Theorem of Holmgren repeated application of (4.3) it follows that L g vT ~ aa(x)D~dx lal<m = J:o ~ (-I)la IDa(v Ta,,(x»)udx+ r M(v,u,ndSx' (4.4) J ao lal<m Here M in the surface integral is linear in the !k with coefficients which are bilinear in the derivatives of v and u, the total number of differentiations in each term being at most m - 1. The expression M is not determined uniquely but depends on the order of performing the integration by parts. This is the Lagrange-Green identity for L which we also write in the form r vTLudx= r (iv)TUdx+ r M(v,u,ndSx, J J (4.5) iv= ~ (- I)1"IDa(aa(x)Tv). lal<m (4.6) Jg where i o ao is the (formally) adjoint operator to L, defined by The simplest example corresponds to the Laplace operator L = tl for scalars u and v. Then one integration by parts yields Jrovtludx= Jrao ~i vUx,!;dS- Jro ~i vrux,dx. -, (4.7) We write this as Jao vddudS-r~vxuxdx. n Jo i " Ivtludx= ( o (4.8) Integrating once more by parts we obtain 1'0vtludx= kutlvdx+ IaJ ~~ v - u ~~ )dSx' (4.9) 5. The Uniqueness Theorem of Holmgren It is clear from the arguments used in the proof of the Cauchy-Kowalewski theorem that an analytic Cauchy problem with data prescribed on an analytic noncharacteristic surface S has at most one analytic solution u, since the coefficients of the power series for u are determined uniquely. This does not exclude the possibility that other nonanalytic solutions of the same problem might exist. However, uniqueness can be proved for the Cauchy problem for a linear equation with analytic coefficients and for data (not necessarily analytic) prescribed on an analytic noncharacteristic surface S. The method of proof (due to Holmgren) makes use of the Cauchy-Kowalewski theorem and the Lagrange-Green identity. (Extension of the uniqueness theorem to nonanalytic equations is much more difficult). 65 3 Characteristic manifolds and the Cauchy problem Figure 3.1 We give a sketch of the Holmgren argument which reduces uniqueness of solutions U(XI""'Xn ) for one problem to existence of solutions of the "adjoint" problem for a dense set of data. Assume we are given an analytic family of hypersurfaces SA depending on a parameter A. for 0..; A...; 1 and such that all SA have a common (n - 2)-dimensional boundary. For 0..; A. < /L"; 1, the surfaces SA'S,. shall fonn the boundary of an n-dimensional region RAw (See Figure 3.1.) All S>.. shall be noncharacteristic with respect to the mth-order linear operator L= ~ Aa(x)Da, (5.1) lal<m where the Aa are analytic in RO]. Holmgren's theorem asserts that a solution of Lu = 0 with Cauchy data 0 on So is detennined uniquely in R OI • Assume we know already that u has vanishing Cauchy data on S>... If there exists for a certain w(x) a solution v of iv=w(x) (5.2) in R>..p' for which on S,. for IPI < m, then (5.3) f wTudx=O (5.4) RA,~ by the Lagrange-Green identity (4.5). If here the w for which a solution v of (5.2), (5.3) exists fonn a dense set* of functions in CO(R>..p) it follows that • The set is dense in the sense that any continuous u can be approximated uniformly by w in the set. 66 6 Distribution Solutions u=O in RAp. and hence also that u has vanishing Cauchy data on S".. Actually the Cauchy-Kowalewski theorem only asserts that for given analytic w there exists a solution v of (5.2) and (5.3) in a neighborhood of Sp. and not necessarily in all of RAp.. However, a closer look (not carried out here; see problem 2 at the end of Section 3) at the proof permits us to show that in the linear case a solution of (5.2) and (5.3) will exist in all of RAp. for all polynomials w provided only that I /L - AI is sufficiently small. Since the polynomials w form a complete set by the Weierstrass approximation theorem, it follows that u = 0 in R}..p.. Dividing now the interval 0« A« I into a finite number of sufficiently small subintervals by points AO=O, Al, ... ,AN= I, we prove successively that u=O in R}..O}..I,R}..I}..Z,R""_I}..N' and hence in all of R01 • 6. Distribution Solutions* The Lagrange-Green identity (4.5) has other applications. The identity reduces to k vLu dx = k (iv) T u dx (6.1) in the case when all boundary terms vanish, e.g., when either u or v have Cauchy data zero. In particular, let Lu=w inn and DfJv=O onanforIPI<m. Then the identity (6.2) (6.3) holds. We can use this identity to define generalized solutions u of Lu=w. For example, if u is continuous we can require this identity to hold for all vE em, vanishing near an. This leads to the notion oj distribution solutions in the sense of Laurent Schwartz. The idea is to replace a functionJ(x) which is defined on an open set n in ~n by the integrals formed with this function for different weights w. We associate with the point function J( x) the Junctional f[ <p] = k<P(x)J(x)dx, (6.4) where <P E 6j) = CoOO(n) is the space of "test functions," that is, functions having derivatives of all orders and compact support. t This Junctional J exists for any continuous or locally integrable Junction J. The integral for J[<p] defines a linear functional on 6j), with values in ~. The values of the functionJ[<p] for varying <P determine the functionJ(x) uniquely whenJ(x) is continuous. Indeed, if the continuous function g is such that J[<P] = g[<p] * ([3], [8], [15]) tTbat is, cj>=O outside a closed and bounded subset of D. Generally, the support of a function cj>(x) is the closure of the set of x for which cj>(x),.,O. 67 3 Characteristic manifolds and the Cauchy problem for all cP E 6j), then, f cp(x)(j(x) - g(x))dx=O (6.5) for all CPE6j). If here f¢g, say f- g>O at a point P, then also in a neighborhood of P; choosing a test function which is nonnegative and vanishes outside this neighborhood would contradict (6.5). Thus f- g=O. Consider next derivatives of f. If f E C l(n) we find by integration by parts (6.6) The left-hand side is obtained by applying the junctional D,j to test functions cpo Thus D,J[cp] = - fIDkCP]. We can use the right-hand side of (6.6) to define the left-hand side when f has no derivative or is not even continuous. As long as the functional associated with f is defined for all test functions cp, the functional associated with D,j makes sense. More generally, we are led to the notion of a distribution. Definition. A distribution is a linear functionalfIcp] defined for all CPE6j) = CoOO(n) which is continuous on 6j) in the following sense: Let the CPr be a sequence in 6j). Then provided (a) all CPk vanish outside the same compact subset of (b) n, and uniformly in x for each a (not necessarily uniformly in a). Each continuous (or even locally integrable) function f(x) generates a distribution f[ cp ] = f cp(x)f(x)dx. (6.7) More generally, we write any distribution f symbolically as k f[ cpJ = cp(x)f(x)dx. (6.8) A specially important distribution, not generated by an integrable point function, is the so-called Dirac function with singularity ~, denoted by 8~, which is defined by (6.9) It is symbolically given by 10cp(x )8~(x)dx =cpW· 68 (6.10) 6 Distribution Solutions Two distributions f[cp] and g[cp] naturally are called equal, if f[cp] = g[cp] for all cp E 6j). More generally we say that two distributions f,g agree in an open subset w of 0 if f[cp] = g[cp] for all cp E 6j) that have their support in w; This permits us in some cases to assign point values to a distribution in a subset of O. Thus for the Dirac function 81< defined by (6.9) we have 8E(x)=0 for xEO, x*~. (6.11) Indeed takingf= 8E, g=O, we havef[cp]= g[cp] =0 for any cp with support in the set w obtained by deleting ~ from O. For a distribution f we define the "derivative" D,J as the distribution given by (6.12) and more generally D af by D"l[ cp ] = ( - I)lalJ[ Dacp ]. (6.13) One easily verifies that formulas (6.12), (6.13) actually define distributions D,J,D&.j. As an example we have from (6.9) that Dk 8l<[cp] = -CPXk(O. In particular, (6.13) yields a definition for derivatives of a continuous function f(x), not necessarily as a function with point values, but as a generalized function for which weighted integrals are defined. Still more generally than (6.13) we can apply any scalar linear differential operator L with C<XJ coefficients to a distribution u(cp), we define the distribution Lu(cp) by Lu[ cp] =u[ £p] (6.14) in accordance with the Lagrange-Green integral formula ~cpLudx= ~{£P)udx (6.15) valid by (4.5) for a test function </> and a scalar function uEC m • (Similar definitions can easily be given for the case where u is a vector, and L corresponds to a system.) We are interested particularly in the distribution solutions L of the equation (6.16) where 81< is the Dirac operator defined by (6.9). They are the so-called fundamental solutions with pole ~ for the operator L. We notice that adding to a fundamental solution u any ordinary solution v E Cm(O) of the homogeneous equation Lv = 0 again yields a fundamental solution. In many cases the equations defining a particular distribution as a linear operator in 6j) define the operator for a much wider variety of functions cp. For example, the operator 8E[cp] can be defined by (6.9) or (6.10) for all functions cp(x) that are just continuous in O. Similarly for an mth-order linear differential operator L with coefficients in Cm(O), we can define Lu(cp) by (6.14) for a locally integrable function u(x) and for cpE Cm(O). More precisely we call u( x) a weak solution of the equation Lu( x) = w( x) in 69 3 Characteristic manifolds and the Cauchy problem n, if f <J>(x)w(x)dx=f (i<J>(x»u(x)dx (6.17) for all <J> E C~(n) (that is for all <J> of class c m with compact support in n)*. Other types of generalized solutions will be encountered in the sequence. EXAMPLE. Let n be the x-axis and L the ordinary differential operator d 2 jdx 2 • Then u(x)=~lx-~1 is a fundamental solution for L. Indeed the distribution associated with u" by (6.13) is L:oo ~lx-~I<J>"(x)dx=<J>(~)= 8€[ u"[ <J> ] = u[ <J>"J = when <J> E <J> ] COOO(IR). PROBLEMS 1. Show that for a continuous function f the expression u = f(x - ct) is a weak: solution of the partial differential equation ut+cux=O. (Hint: Transform for <p E CJ(1R2) the integral f f (<pt+c<Px)udxdt to the coordinates YI = X - ct, Y2 = x.) 2. Show that the function U(X\>X2) defined by U (X I, X )= { I 2 0 for XI >~I' x2>~2 for all other X\>X2 is a fundamental solution with the pole (~I' ~2) of the operator L = a2/ ax I aX2 in the xlxrplane. 3. Show that the function u ( XI,X2 ) = { ! 2 o forlxl-~d<~2-x2 otherwise is a fundamental solution for L=(a2/ax~)-(a2/ax?) with pole (~1'~2)' 4. Verify the special cases of Green's identity (6.18) dv du d/).v) dS. v--/).u-+/).v--uLo(v/).u-u/).v)dx= iao (d/)'U dn dn dn dn 2 2 * It is sufficient to require (6.17) to hold for all </> E 6j) since every mated uniformly with its derivatives of order .;; m by </> E 6j) • 70 </> E (6.19) C{)' can be approxi- 6 Distribution Solutions 5. Show from Holmgren's uniqueness theorem that a solution u(X,y,z,/) of the wave equation Ult = c2( Uxx + ~y + uzz ) at the point (0,0,0, T) is determined uniquely by its Cauchy data on x2+y2+z2<c 2T2, 1=0. (Hint: Take for the S suitable hyperboloids of revolution about the I-axis passing through X2+y2+z2=c 2T2, 1=0.) 71 4 The Laplace equation * 1. Green's Identity, Fundamental Solutions, and Poisson's Equationt The Laplace operator acting on a function u( x) = u( X I' ••• ,xn ) of class C 2 in a region Q is defined by n d= ~ k=! Df (1.1) For u,v E C 2 (Q) we have:!: (see Chapter 3, (4.8), (4.9» Green's identities. where d / dn indicates differentiation in the direction of the exterior normal to ClQ. The special case v = I yields the identity r dudx= JrafJ ddun dS. JfJ (1.3) *([2]. [6]. [11]. [13]. [14]. [14]. [23]. [26D t({17D *We assume here that Chapter 3. is valid. 72 n is an open bounded set, for which the divergence theorem, (4.1) of I Green's Identity, Fundamental Solutions, and Poisson's EqUation Another special case of interest is v=u. We find then from (1.2a) the energy identity r~ u~dx+ JrouAudx= Jrao u un ~u dS. Jo i (1.4) If here Au = 0 in Q and either u = 0 or du / dn = 0 on aQ, it follows that r ~i u;dx=O. ' Jo (1.5) For u E C 2(n) the integrand is nonnegative and continuous, and hence has to vanish. Thus u = const. in Q. This observation leads to uniqueness theorems for two of the standard problems of potential theory: The Dirichlet problem: Find u in Q from prescribed values of Au in Q and of u on aQ. The Neumann problem: Find u in Q from prescribed values of Au in Q and of du / dn on aQ. As always in discussing uniqueness of linear problems, we form the difference of two solutions, which is a solution of the same problem with data O. We find that the difference is a constant, which, in the Dirichlet case, must have the value O. Thus: A solution u E c 2(n) of the Dirichlet problem is determined uniquely. A solution u E C 2(n) of the Neumann problem is determined uniquely within an additive constant. (Notice also that the solution of the Neumann problem can only exist if the data satisfy condition (1.3». One of the principal features of the Laplace equation Au=O (1.6) is its spherical symmetry. The equation is preserved under rotations about a that is under orthogonal linear substitutions for x-~. This makes it plausible that there exist special solutions v(x) of (1.6) that are invariant under rotations about ~, that is have the same value at all points x at the same distance from ~. Such solutions would be of the form point~, v=l[;(r), (1.7) where (1.8) represents the euclidean distance between x and ~. By the chain rule of differentiation we find from (1.6) in n dimensions that I[; satisfies the ordinary differential equation n-l Av= I[;"(r) +-I[;'(r) =0. r (1.9) 73 4 The Laplace equation Solving we are led to (1.10a) I//(r) = Cr 1 - n Cr2-n I/;(r)= { 2-n Clogr whenn>2 (1.10b) whenn=2 (1.1Oc) with C = const., where we can still add a trivial constant solution to 1/;. The function v(x)=I/;(r) satisfies (1.6) for r>O, that is for x+~, but becomes infinite for x=~. We shall see that v for a suitable choice of the constant C, is a fundamental solution for the operator d, satisfying the symbolic equation, (see Chapter 3, (6.16)), (1.11) Let u E C 2(Q) and ~ be a point of n. We apply Green's identity (1.2b) with v given by (1.7), (1.10b,c). Since v is singular at x=~ we cut out from 12 a ball B(~,p) contained in 12 with center ~, radius p, and boundary S(~,p). The remaining region np = 12 - B(t p) is bounded by an and S(~, p). Since dv = 0 in np we have r vdudx= JrafJ (v dudn -u dn. dv )dS+ r J JfJ S(g,p) p (v du -u dV)dS. dn dn np Here on S(~,p) the "exterior" normal to our region Consequently by (1.10a,b,c), (1.3) points towards v = I/;(p), J.r S(g,p) du vTdS=I/;(p) n r f ~. (1.13a) S(g,p) Tdu dS = -I/;(p) n u dv dS= - Cpl-n JS(g,p) dn (1.12) r JS(g,p) f B(g,p) udS. dudx (1.13b) (1.13c) Since both u and du are continuous at ~ the right-hand side of (1.13b) tends to 0 for p~O by (1.10b,c), while that of (1.l3c) tends to - CWnu(~), where Wn denotes the surface "area" of the unit sphere in IRn. [The values W2-2'IT, w3=4'IT are familiar; generally Wn =2Y7T n/r(~n)]. Thus (1.12) becomes for p~O (note that v, though 74 00 at x=~, is integrable near ~. We now choose I Green's Identity, Fundamental Solutions, and Poisson's Equation C= ljwn in (1.10b,c), so that 1/I(r)={ (2::;W logr for (USa) n>2 n for n=2. 2'11" We write the corresponding v in its dependence on x and (USb) ~ as v = K(x,~) = 1/I(r) = 1/1(1 x -~I). (1.16) Then (1.14) becomes u(~)= Jr K(x,~)Audx- Jr (K(X'~) d~(x) -u(x) dKd,X'~) )dSx (1.17) un nx o ao x for ~E~, where the subscript "x" in Sx and dnx indicates the variable of integration respectively differentiation. (Notice that for ~ e: D the left-hand side of identity (1.17) has to be replaced by O. This follows from (1.2b), since v=K(x,~EC2(D) and Av=O for ~ outside D.) Taking in particular for u in (1.17) a test function </> E COoo(~), we find that f </>(~)= K(x,~)A</>(x)dx Hence v = K(x,~ (1.18) defines a distribution for which v[ A</> ] = </>(~). Since L=A is (formally) selfadjoint (that is L=L), we can interpret (1.17) as stating that the functional vA applied to a test function </> has the value </>(~) (see Chapter 3, (6.15», or that v in the distribution sense satisfies (1.11), and is a fundamental solution with pole ~. Let uE C 2(D) be "harmonic" in~, that is, be a solution of Au=O; then by (1.17) for ~E~ u(~)= - r (K(X'~) dUdnx(x) -u(x) dKd,X'~) )dSx. nx J ao (1.19) Formula (1.19) expressing u in ~ in terms of its Cauchy data u and dr!i dnx on a~ represents the solution of the Cauchy problem for ~, provided such a solution exists. Actually, by the uniqueness theorem for the Dirichlet problem proved earlier a solution of Au = 0 is determined already by the values of u alone on a~. Thus we cannot prescribe* both u and du j dnx on a~. The Cauchy problem Jor the Laplace equation in ~ generally has no solution. Formula (1.18), however, is useful in discussing regularity of harmonic functions. Since K(x,~)=1/I(lx-~D is in Coo in x and ~ for X=F~, we can form derivatives of u with respect to ~ of all orders under the • The Cauchy data cannot even be prescribed as arbitrary ana(ytic functions on aD. This does not contradict the Cauchy-Kowalewski existence theorem, since here we require u to exist in all of D, and not just in a sufficiently small neighborhood of aD. 75 4 The Laplace equation integral sign for ~ E~, and find that u E C oo(~). More precisely, we can even conclude that u(~ is real analytic in ~. To see this we only have to continue u suitably into a complex neighborhood. We observe that K = t/!(r), with r given by the algebraic expression is defined and differentiable for complex x,~ as long as r+O. In particular r+O when x is confined to real points on im and ~ to complex points in a sufficiently small complex neighborhood of a real point of ~. Formula (1.19) then defines u(O as a differentiable function of ~ in that complex neighborhood. It follows that u is real analytic in the set ~. We need not assume that u E C 2(U). To belong to Coo or to be analytic is a "local" property. A solution of the Laplace equation in any open set ~ is of class C 2 in any closed ball contained in ~ and hence real analytic in the open ball. Thus harmonic functions are real analytic in the interior of their domain of definition. We can show from this that the Cauchy problem for the Laplace equation generally is unsolvable, even locally. Take for the initial surface a portion (1 of the plane xn = O. Prescribe the Cauchy data u=O, (1.20) on (1. Let ~E (1 and let B be a ball with center ~ whose intersection with Xn = 0 lies in (1. Denote by B + the hemispherical portion of B lying in xn ;) O. There cannot exist a solution u of the Laplace equation of class C 2 in jj + with Cauchy data (1.20) for xn = 0, unless g is real analytic. To see this one continues u into the whole of B by reflection, defining u(x)= u(x1, ... ,xn) for xEB with xn<O by (1.21) One easily verifies that the extended u belongs to C 2(B); (the values of u and its first and second derivatives fit the reflected values along xn = 0, because u=~u=O there). Moreover, ~u=O in B, since the Laplace equation is unchanged when we replace u by - u or Xn by - Xn. Consequently u is real analytic in the whole of B. In particular then ux,,(x1, ... ,Xn_I,0) is a real analytic function of XI"'" Xn - I' Let w(x)=w(xl, ... ,xn) be any solution of ~w=O of class C 2(U). Then G(X,~) = K(x,~) + w(x) (1.22) again is a fundamental solution of the Laplace equation with pole ~. (See Chapter 3, p. 69.) More precisely identity (1.17) stays valid when we 76 I Green's Identity, Fundamental Solutions, and Poisson's Equation replace K by G: 1 u(g) = n G(x,g)tludx- i m (G(X,g) d~(x) ~ as follows immediately from (1.17), (1.2b). As an application we take the case where and radius p, choosing for G the function Then on u(x) dGd;,g) )dSA1.23) x n is a ball B(g,p) of center g an dG _.//(p)_ - -1p I-n , dnx Wn G=O, --'t' and (1.23) becomes u(g)= I Ix-gl<p (1[;(lx-gj}-1[;(p»tlu(x)dx+ In_I WnP I Ix-fl=p u(x)dSx • (1.2S) For tlu=O this is Gauss's law of the arithmetic mean: u(g) In_I WnP I Ix-fl=p u(x)dSx ' (1.26) where wnpn-I is the surface area of the sphere Ix-gl=p. In words: For a function u harmonic in a closed ball the value of u at the center equals the average of the values of u on the surface. Since the 1[;(r) given by (1.1Sa,b) is a monotone increasing function of r for all dimensions n, we obtain more generally from (1.25): If tlu(x) ~ 0 in the ball Ix -gl .,;; p, then u(g).,;; In_I WnP I Ix-gl=p u(s)dSx ' (1.27) A function u cont41uous in n is called subharmonic, if for each gEn the inequality (1.27) holds for all sufficiently small p. Thus functions in C 2(n) with tlu";; 0 are subharmonic. Formula (1.18) expresses that K(x,g) is a fundamental solution for tl. Another aspect of this property is Poisson's formula (1.28) vaiid for u E C 2(U) and gEn. Here tl€ denotes the Laplace operator taken with respect to the variables g. Thus for given u E C 2(U) we have in w(g) = ~ K(x, g)u(x) dx (1.29) 77 4 The Laplace equation a special solution w of the inhomogeneous Laplace equation ("Poisson's differential equation") (1.30) ~~w(~)=u(~) for ~EQ. Formally (1.28) follows directly from (1.16), (1.11): ~~f K(x,~)u(x)dx= f (~~lHlx-W)u(x)dx = f (~A(lx-~I»u(x)dx = f 8~(x)u(x)dx= u(~). For a rigorous derivation we first assume that u E CJ(Q). Then by (1.17) for ~ E Q, since u = 0 near aQ, L u(~)= K(x'~)~xu(x)dx= f K(x'~)~xu(x)dx. (1.31) (As always the domain of integration is the whole space, when no other domain is indicated). Actually (1.31) holds for all ~, since for given u E CJ(Q) nothing changes when Q is replaced by any larger open set containing~. Withy=x-~ as variable of integration we have by (1.16) u(~)= f l{I(lx-W~xu(x)dx= f l{I(lyi)~u(y+~)t6-' =f l{I(IYI)~~u(y +~)t6-' =~~f l{I(lyi)u(y +~)t6-' =~~f K(x,~)u(x)dx confirming (1.28). Let next u E C 2(Q). Let b be any ball with ii c Q. We can find a concentric ball B such that ii c B, jj c Q, and a "cutoff function" nx)ECJ(Q), which has the value 1 everywhere in B. (See Figure 4.1.) Then where ru u=ru+(I-nu, E CJ(Q) and (1vanishes in B. Thus for ~ E b nu ~"L K(x,~)Hx)u(x)dx= rwu(~)= u(~) ~~ r K(x,~)(l- Hx»u(x)dx =~" r J~ J~-B (1.32a) K(x,~)(I - r(x»u(x)dx=O, (1.32b) since K(x,~) is regular and harmonic in ~ for xEQ-B, ~Eb. Adding (1.32a,b) yields (1.28) for ~ in any b, and hence for all ~EQ. For ~ outside Q we find by direct differentiation under the integral sign that ~~w(~)=O for the w defined by (1.29). For ~ on aQ the second 78 1 Green's Identity, Fundamental Solutions, and Poisson's Equation ~=O I / / / / .".- I \ \ "'" - '""'---- ----' Figure 4.1 derivatives of w({l may cease to exist. One easily verifies however that C l(lRn), since the first ~-derivatives of K( x,~) are still integrable with respect to x. w(~) E PROBLEMS 1. Let u belong to C 2(Q) and be subharmonic. Show that au ;;.0. [Hint: Use (1.25).] 2. Let L=a+c in n=3 dimensions, where c=const. (L="reduced wave opera- tor"). (a) Find all solutions of Lu=O with spherical symmetry. (b) Prove that K(x,~)= _ cos~Vc r) , wr (1.33) is a fundamental solution for L with pole ~. Show that for a solution u of Lu=O formula (1.19) holds with K defined by (1.33). [Hint: Use formula (6.18) of Chapter 3.] (c) Show that a solution u of Lu = 0 in the ball Ix - ~I ;;;; p has the modified mean value property u(~)= 1 Vc p ~ u(x)dSx • sin(Vc p) 4wp Ix-EI=p (1.34) (Here for c = - y < 0, the factor Vc p/sin(Vc p) stands for Vy p/sinh(Vy p).) [Hint: Use the fundamental solution (1.35) with a suitable constant k.] 79 4 The Laplace equation (d) Show that a solution u of Lu=O of class C 2(U) vanishing on ao vanishes in 0, provided c < O. Show that for c > 0 there are solutions vanishing on a sphere but not in the interior. (e) Show that solutions of Lu=O in 0 are real analytic in O. 3. (a) Show that for n=2 the function v=_1 r 210gr r=lx-~1 (1.36) 8'IT ' is a fundamental solution for the operator /)/. [Hint: dv=(1 + logr)/2'IT.] (b) Show that for u E C 2(U) and ~ E 0 u(~)=lvd2udx-r (vddU_dUdv+dVdu_uddV)dS. o Jao dn dn dn dn (1.37) [Hint: Apply (1.2b) with u replaced by dU, and use (1.17).] 4. (a) Find all solutions with spherical symmetry of the biharmonic equation d2u=o in n dimensions. (b) Find a fundamental solution. S. Prove that u(x)=u(xJ> ... ,xn)=O also implies that (1.38) d(lxI2- nU(x/lxI2») =0 for x/lxl2 in the domain of definition of u. 6. Let x,y denote coordinates in the plane. Let u(x,y) be a solution of the two-dimensional Laplace equation Uxx + Uyy = 0 in an open simply connected set O. (a) Prove that there exists a conjugate harmonic function v(x,y) such that the Cauchy-Riemann equations ux=Vy, (1.39) Uy= -Vx are satisfied. [Hint: for a fixed point (xo,Yo) in 0 define v by (1.40) where the integral is taken along any path joining (xo,Yo) to (x,y).] (b) Introduce the complex-valued function f = u + iv of the complex argument z = x + ry. Prove Cauchy's theorem that for any closed curve C in 0 I f(z) dz = Ie (u + iv)( dx + idy) = O. [Hint: There exist functions q,(x,y), 1jJ(x,y) in 0 with dq,=udx-vdy, d!V=vdx+udy.] 7. By Newton's law the gravitational attraction exerted on a unit mass located at ~= (~1>~2'~3) by a solid 0 with density JL = JL(x) is given by the vector F(~)=y Iff JL(X)(X-~) o (y = universal gravitational constant). 80 Ix-~13 dx 2 The Maximum Principle (a) Prove that F= gradu, where the "potential" u is given by u(~)=Yfff p.(x) dx. Ix-~I (b) Prove that the attraction F(f> exerted by 0 on a far away unit mass is approximately the same as if the total mass of 0 were concentrated at its center of gravity xO= f fDf p.(x)xdx/ f fDf p.(x)dx. [Hint: Approximate 1~-xr3 by 1~_xol-3 for large I~I.] (c) Calculate the potential u and attraction F of a solid sphere 0 of radius a with center at the origin and of constant density p.. Use here that u must have spherical symmetry, must be harmonic outside 0, satisfy Poisson's differential equation in 0, be of class C 1 everywhere, and vanish at 00. [Answer: u(~)=2'ITyp.a2-~'lT'Yp.1~12 for 1~I<a,u(f>=~'lT'Yp.a31~1-1 for 1~I>a.] 8. Let u, v be conjugate harmonic functions satisfying (1.39) in a simply connected region O. Show that on the boundary curve ao du dv dv du dn=ds' dn=-ds' where dn denotes differentiation in the direction of the exterior normal and ds differentiation in the counterclockwise tangential direction. Show how these relations can be used to reduce the Neumann problem for u to the Dirichlet problem for v and conversely. 2. The Maximum Principle One of the important tools in the theory of harmonic functions is the maximum principle. Similar principles hold for solutions of more general second-order elliptic equations, and for complex analytic functions. In this section we assume that ~ is a bounded, open, and connected set in Rn. We first prove a weak Jorm oj the principle: Let u E C 2(O) n CO(Q), and let flu ;;. 0 in O. Then maxu=maxu. fi aD (2.1) (Notice that a continuous function u assumes its maximum somewhere in the closed and bounded set D. Formula (2.1) asserts that u assumes its maximum certainly on the boundary of ~, possibly also in ~.) Indeed under the stronger assumption flu>O in~, relation (2.1) follows from the fact that u cannot assume its maximum at any point ~E~; for then a2u / ax~ '" 0 at ~ for all k, and hence flu '" O. In the case flu ;> 0 in ~ we make use of the auxiliary function v=lxl 2 for which flv>O in~. Then for any constant e > 0 the function u + w belongs to C2(~) n CoCO), and satisfies fl(u+w»O in~; hence max(u+w)= max(u+w). Li aD 81 4 The Laplace equation Then also maxu+eminv< maxu+emaxv. n n an an For e~O we obtain (2.1). In the special case where u is harmonic in g, relation (2.1) also applies to - u. Since minu = - max( - u) we obtain min u = min u. n (2.2) an These relations imply a maximum principle for the absolute value (using that lal =max(a, - a) for real a): If u E C 2(g) n Co(U) and ~u = 0 in g, then maxlul= max lui. n an (2.3) In particular u = 0 in g if u = 0 on ago This implies an improved uniqueness theorem for the Dirichlet problem (see p. 73) not requiring u to have derivatives on the boundary: A function u E C 2(g) n Co(U) is determined uniquely by the values of ~u in g and ofu on ago Stricter versions of the maximum principle flow from the mean value theorem (1.27): Let u E C 2(g) and ~u ~ 0 in g. Then either u is a constant or u(~) <sup u n for all ~Eg. (2.4) More generally (2.4) holds for any nonconstant u that is subharmonic in g. For the proof we set M=supu, and decompose g into the two disjoint sets The set g2 is open because of the continuity of u. Using the fact that u is subharmonic we can show that gl is open as well. For if ~Egl' we have from (1.27) for all sufficiently small p 0<1 Ix-~I=p = I u(x)dSx-Wnpn-lu(~) Ix-~I=p (u(x)-u(~)dSx= I Ix-~I=p (u(x)-M)dSx· Since u( x) - M is continuous and <0, it follows that u( x) - M = 0 on every sufficiently small sphere with center ~. Hence all x in a neighborhood of ~ 82 2 The Maximum Principle belong to ~l' and ~l is open. By definition a connected open set cannot be decomposed into two disjoint open nonempty sets. Thus either ~l or ~2 is empty, proving the principle. As an immediate consequence we have: IfuEC2(~)n CO(U) and ilu;;;'O in~, then either u=const. or u(~) <max u an (2.5) for all ~ E~. Again (2.5) holds more generally for all u that are continuous in U and subharmonic in ~. (We need only observe that max u cannot be assumed at a point of ~.) PROBLEMS 1. Let Q denote the unbounded set JxJ > 1. Let uE C 2(n), Llu=O in Q, and limx->cou(x)=O. Show that max JuJ = max u. aD ~ [Hint: Apply maximum principle to spherical shell.] 2. Let u( x) E C 2(Q) n C 0(0) be a solution of n (2.6) Llu+ ~ ak(x)ux +c(x)u=O, k=l k where c(x) <0 in Q. Show that u=o on aQ implies u=O in Q. [Hint: Show that maxu.;; 0, minu ~ 0.] 3. Prove the weak maximum principle (2.1) for solutions of the two-dimensional elliptic equation Lu = auxx + 2buxy + cUyy + 2dux + 2ezs, = 0, (2.7) n where a,b,c,d,e are continuous functions of X,Y in with ac-b 2 >0,a>0. [Hint: Prove first the maximum princip'le for solutions of Lu > 0, using that at a maximum point in Q lIyy .;; o. Apply this to u + ev where v=exp[ M(x-xoi+(Y-Yoi)], with (xo,Yo) outside Q and M sufficiently large.] 4. Let n = 2 and Q be the half plane X2 > O. Prove the maximum principle (2.3) for u E C 2(Q) n Co(n) which are harmonic in n, under the additional assumption that u is bounded in (The additional assumption is needed to exclude examples like u = X2') [Hint: Take for E > 0 the harmonic function n. U(Xb X2)- elogylX?+(X2+ 1)2 . 83 4 The Laplace equation Apply the maximum principle to a region Let e~O.] Xr+(X2 + 1)2 < a 2,X2;;' 0 with large a. 3. The Dirichlet Problem, Green's Function, and Poisson's Formula We derived the representation (1.23) for u in terms of Cauchy data, involving a fundamental solution G(x,~. If here G(x,~=O for xEan and ~ E n, the term with du / dnx drops out and we have solved the Dirichlet problem. We call a fundamental solution G(x,~) with pole ~ a Green's function (for the Dirichlet problem for the Laplace equation in the domain n), if (3.1) for XEQ, ~En, x~~, with K defined by (1.16), (1.15a,b), where v(x,~ for ~En is a solution of Axv=O, of class C 2(Q), for which G(x,~)=O for xEan, ~En. (3.2) To construct G in general we have to find a harmonic v with v = - K on an, which is again a Dirichlet problem. However in some cases G can be produced explicitly. This in particular is the case when n is a halfspace or a ball; then G can be obtained by reflection, leading to Poisson's integral formula. We note that for n=2 the Laplace equation is invariant under conformal mappings. Thus if we can solve the Dirichlet problem for a circular disk, we can solve it for any region which can be mapped conformally onto a disk. To derive Poisson's integral formula for the solution of the Dirichlet problem for the ball of radius a and center 0, n= B(O,a) = {xllxl < a}, (3.3) we make use of the fact that the sphere an is the locus of points x for which the ratio of distances r=lx-~1 and r*=lx-~*1 from certain points ~ and ~* is constant. Here for ~ we can choose any point of n. Then ~* is the point obtained from ~ by "reflection" with respect to the sphere an, that is, (3.4) One easily verifies that r* a (35) -;:-=m=const. for xEan. For n > 2 the fundamental solutions with poles I 2-n K( x,o;;~) (2-n)w n r, 84 ~ K( ~*)_ X,o;; - and ~* I r*2-n (2-n)wn 3 The Dirichlet Problem, Green's Function, and Poisson's Formula are then related for x E a{l by K(x,~*)= ( IDa )2-nK(x,~). Thus the function (3.6) vanishes for x E a{l. Moreover the second term is singular only when n, the function K(x,~*) is harmonic in x throughout n. Thus G is a Green's function and formula (1.23) applies for u E C 2(n). In the special case where ~u = 0 in the ball {l, and u E C 2(n) we find, after a simple computation, Poisson's integral formula x=~*. Since ~* lies outside u(~)= valid for I~I IIxl=aH(x,~)u(x)dSx (3.7) < a. Here H, given by _ I a2_1~12 H(x,~) - - I I:.ln , aWn x-,. (3.8) is the Poisson kernel. We arrive at the same formula for n=2. For given boundary values u = f on a{lJormula (3.7) solves the Dirichlet problem, provided that problem has a solution U E C 2(n). We shall verify directly that for f continuous on a{l the problem actually has a solution given by Poisson's formula: Let f be continuous for for I~I = a and by Ixl = a. u(~)= Then the function u(~) given by fm IIxl=a H(x,~)f(x)dSx (3.9) for I~I < a, is continuous for I~I..;; a, and in Coo and harmonic for 1~I<a. The proof follows easily from the following properties of H: for Ixl";;a, 1~I<a, (b) ~~H(x,~=O for 1~I<a, Ixl=a. (c) flxl_aH(x,~dSx=1 for 1~I<a. (d) H(x,~>O for Ixl=a, I~I <a. (e) If Irl=a, then (a) H(x,~ECOO lim ~-+~ x~~. H(x,~)=O IEI<a uniformly in x for Ix - r I> 8 >O. 85 4 The Laplace equation Here properties (a), (d), (e) are clear by inspection of (3.8). Property (b) follows either from (3.8) or by ·observing that G(x,~) as defined by (3.6) is harmonic in x, that (3.10) G(x,~)= G(~,x), and that H(x,~)=dG(x,~)/dnx. To derive (c) directly would be tedious; but (c) follows simply by applying (3.7) to the function u(x) = 1, which is harmonic and has boundary values 1. By differentiation under the integral sign we find immediately from (a), (b) that the u(~ defined by (3.9) belongs to C<X> and is harmonic for I~I < a. There remains to prove the continuity of u for I~I..;; a. Let Ir I= a, I~I < a. By (c) uW-fG)= ~xl=aH(X,~)(j(x)-f(n)dSx (3.11) =/\ +/2 , where f f ... , Ix-~1<6 Ix-~1>6 Ixl=a Ixl=a For a given 10 > 0 we can choose 8 = 8 (e) > 0 so small that If(x)-f(nl<e for Ix-rl<8, Ixl=a, since f is continuous. Then lId";; 10 by (c), (d). Let maxi f(x) I= M for Ixl = a. By (e) we can find a 8' such that 10 H(x,~)< \ forl~-rl<8',lx-rl>8, (3.12) 2Mwn a n where 8' depends on 10 and 8=8(10), and hence only on e. (See Figure 4.2.) Then also 1/21 < e. Hence lu(~)- f(nl <210 for I~- rl <8', I~I <a, which shows that u is continuous at the boundary point r. This completes the proof of the theorem. As an application we derive estimates for the derivatives of a harmonic function u in terms of estimates for u. We take at first the situation, where ~ is the balllxl < a, where u E C 2(n), and Au = 0 in ~. Using (3.7), (3.8) we find by a simple computation that (3.l3a) and hence that lu;(O)I..;;~ max lu(x)l. , 86 a Ixl=a (3.l3b) 3 The Dirichlet Problem, Green's Function, and Poisson's Formula Figure 4.2 Let next au=O in any open set Q. Let gEQ and let g have distance d(~ from the boundary aQ. We apply (3.13b) to a ball of any radius a < d(~ with center at g. For a~dm we obtain the inequality (3.13c) Similar inequalities obviously hold for higher derivatives also. Let w denote a compact subset of Q. Then there exists a positive lower bound for d(~ in w. All harmonic U with a common upper bound M for lui in Q, will have a common upper bound in w for the absolute values of their derivatives up to a fixed order. The inequalities for derivatives of u in terms of u lead to completeness and compactness properties of the set of harmonic functions. Let there be given a sequence Uk E C 2(Q) n Co(U) satisfying aUk = 0 in Q. Assume first that the Uk converge uniformly on aQ towards a function f. Then the Uk converge uniformly in n to a continuous function u by the maximum principle. In any compact subset w of Q for a fixed multi-index a the derivatives D "Uk converge uniformly to D "u. Hence u E C OO(Q) and au = O. (We conclude in particular that uniform limits of harmonic functions are again harmonic.) Under the weaker assumption that lukl..;; M on aQ for all k, we have a common bound for the Uk and their first derivatives in the compact subset w. By Arzela's theorem there exists then a subsequence of the Uk which converges uniformly in w towards a function u. We conclude as before that u is harmonic in w. 87 PROBLEMS 1. Verify the symmetry property (3.10) for the Green's function (3.6). 2. Let n=2 and 0 be the halfplane x2>0. For ~=(~l>~~ define by reflection ~.=(~l> -~~. . (a) Show that G(x,O=K(x,O-K(x,~·) is a Green's function for O. Derive formally the corresponding Poisson formula u(~) = u(~ ,~ ) = 1. I 2 'Ir f 00 -00 ~d(xl) (xl-~1)2+~l (3.14) dx . I (b) Show that (3.14) actually represents a bounded solution of the Dirichlet problem for 0, if j(XI) is bounded and continuous. (c) Show that the maximum principle is satisfied by the solution (3.14) (see problem 4 of Section 2). 3. For n=2 find a Green's function for the quadrant reflection. XI >0, X2>0 by repeated 4. (Liouville's theorem.) Prove that a harmonic function defined and bQunded in all of Rn is a constant. [Hint: Apply (3.13c) to balls of increasing radius.] 5. Let 0 be the halfspace Xn > O. If u E C 2(0) n COCO), ~u =0 in 0, u =0 on a~, and u is bounded in 0, then u=O (In the "counter-example" U=Xn the function u is not bounded). [Hint: Continue u as an odd function of Xn into all of lin.] 6. Letf((1) be a C 4-function of period 2'1r with Fourier series 00 f«(J)= ~ (ancos(n(J)+bnsin(n(J». n=O (a) Prove that 00 • (3.15) u= ~ (ancos(n9)+bnsin(n(J»rn n=O represents in polar coordinates r,(J the solution of the Laplace equation = 0 in the disk X2 +y2 < 1 with boundary values f. (b) Derive Poisson's integral formula (3.7), (3.8) for n=2 from (3.15) by substituting for the 0", bn their Fourier expressions in terms of f and interchanging summation and integration. ~u 7. (Harnack's inequality.) Let uEC 2 for for Ixl < a. Show that for I~I < a Ixl<a, uEC o for Ixl";a, u~O, ~u=O a n- 2(a -I~D u(O)..; u(~)..; a n- 2 (a+ I~I) u(O). (a+I~Dn-1 (a-I~lt-1 (3.16) 8. Show that the constant n in the inequality (3.13b) can be replaced by 'In 2nwn _1 (n-l)wn (3.17) and that this is the smallest possible constant in the inequality. [Hint: Use u=lxnl on Ixl=a in (3.13a).] 88 4 Proof of Existence of Solutions for the Dirichlet Problem 9. Let Au(x) = 0 and lu(x)l.;;;; M for (a) Show that Ix-~I <a. (3.18) where Yn is defined by (3.17) for dimension n. [Hint: Apply (3.13c) successively to the kth derivatives in the balls Ix-~I.;;;; a(m-k)/m for k= O,l, ... ,m-l.] (b) Show that u(x) is repres..nted by its series in terms of powers of x-g for (3.19) 4. Proof of Existence of Solutions for the Dirichlet Problem Using Subharmonic Functions ("Perron's Method") The proof is based on the fact that we can characterize the solution w of the Dirichlet problem by an extremal property; we only have to prove that a function with the extremal property exists. Assume we had a function WEC 2(U)n CO(Q), such that aw=O in U and that w takes the prescribed values j on au. Let u be any function which is subharmonic in U and continuous in Q, for which u <J on au. Then u - w .;;;; 0 on au, and hence u - w .;;;; 0 in U by the maximum principle for subharmonic functions on p. 82. Thus the value of the solution w of the Dirichlet problem at any point ~ of U is the largest value taken at ~ by any subharmonic function with boundary values .;;;; j, and this will be our extremal property. The construction of w from its extremal property proceeds by a number of easily verified elementary lemmas. Essential use is made of the maximum principle and of the solvability of the Dirichlet problem for a ball, assured by Poisson's integral formula (3.7), (3.8). This somewhat limits the extension of the method to more general partial differential equations. In what follows we denote again by B(~,p) the open ball of center ~ and radius p in Rn , by jj(~,p) its closure, and by S(~,p) its boundary. For a continuous u = u(x) we denote by -I. i-n Mu(~'p)=-P Wn S(~,p) u(x)dSx (4.1) the "arithmetic mean" of u on S(~,p). We consider an open, bounded, and connected set U in Rn. In accordance with our previous definition we call u subharmonic in U, if u E CO(U), and if for every ~ in U the inequality (4.2) holds for all sufficiently small p. We denote by o(U) the set of functions subharmonic in U. The maximum principle proved on p. 82 constitutes 89 4 The Laplace equation Lemma I. For uEO'(O)n CO(n) we have (4.3) maxu";; maxu. n an Definition. For uECo(O) and jj(~,p)cO we define Ut;,p as that function in CoCO) for which u€,p(x)=u(x) axu€,p(x)=O for xEO, xtlB(~,p) (4.4a) (4.4b) for xEB(~,p). (That is, u~,p is obtained from U by replacing U in the ball B(~, p) by the harmonic function that agrees with U on the boundary of the ball. The existence and uniqueness of u has been established earlier.) Lemma II. For uEO'(O) and jj(~,p)EO we have u(x)..;; u€,p(x) (4.5a) for all x EO (4.5b) u€,p EI.J(O). PROOF. By definition (4.5a) holds for x tl B(~, p), with the equal sign. With u also its restriction to B(~,p) is subharmonic in B, and so is the harmonic funct~n - uE,p' Thus u- uE,p EO'(B(~,p». Since u- uE,p is continuous in the ball B(~,p) and vanishes on its boundary, it follows from Lemma I that u- uE,p";; 0 in B(~,p), which establishes (4.5a). In order to prove (4.5b) we have to show that for any ~EO uE,p(O..;; Mu!,p (r,'T) r (4.6) for all sufficiently small 'T. Now this is true for tljj(~,p) by (4.4a), since uEO'(O), and is true for EB(~,p) since then uE,p is harmonic near There remains the case where ES(~,p). But then by (4.2), (4.5a) r r Ug,p(r) = u(r)..;; Mu(r,'T)";; Mu!,p (r,'T) r. (4.7) for all sufficiently small 'T. Lemma m. For UE 0'(0) inequality (4.2) holds whenever ii(~, p) cO. PROOF. By (4.4a), (4.5a) and the mean value theorem for harmonic func- tions Lemma IV. A necessary and sufficient condition for U to be harmonic in 0 is that both u and - u belong to 0'(0). PRoOF. The necessity is implied by the mean value theorem for harmonic functions. Let, on the other hand, u E 0'(0), - u E 0'(0). Then for jj(~, p) cO 90 4 Proof of Existence of Solutions for the Dirichlet Problem by Lemma III U(x)..;; U~,p(x), -U(x)";;-U~,p(x) forxEn. D Thus u=u~,p; hence U is harmonic in B(~,p). Lemma IVa. If UE Co(n), and if for each ~En u(~)=Mu(~'p) for all sufficiently small p, then U is harmonic in PROOF. n. The assumptions imply that UE o(n), - UE o(n). D Definition. For f E CO(an), define OJ(Q) = { ulu E CD(Q) n o(n), u";;f on an} (4.8) wix)= sup u(x) for xEn. (4.9) UEOf (£!) Set m=inff, (4.10) f.L=supf· Wf?.. observe that the constant m belongs oIQ), and hence that the set oln) is not empty. Also by Lemma I (4.11) u(x)..;; f.L for UEOj(Q), xEQ. Thus Wj is well defined. Lemma V. Let u1"",ukEoIQ) and v=max(u1,,,,,Uk)' Then vEo/Q). PROOF. One easily verifies that vECD(Q), since u1"",UkECD(Q). Then by (4.2) for any ~En and all sufficiently small p. v(~) =max(ul(g), ... , Uk(~» ..;; max(MUl(~'P), ... ,MUk (~,p»)..;; Mv(~'p)· Lemma VI. Wj is harmonic in D n. Let jj(~,p)cn. Let xI,x 2 , ... be a sequence of points in B(~,p') where p'<p. By (4.9) we can find functions uk EOj(Q) for k,j=I,2,3, ... such that PROOF. (4.12) Relation (4.12) is preserved if any >ufc in n, since then ui is replaced by any U E o/Q) for which U 91 4 The Laplace equation Define the sequence uj(x) for xE~,j= 1,2, ... by uj(x) =max( u{(x), ... ,uj(x)). Then ~ E a/~) by Lemma V and uj(x) ~ u[(x) for x Efl,j ~ k. Thus ~imuj(Xk)=wf(Xk) forallk. (4.13) J-+OO Replacing, if necessary, ~ by max(uj,m), we can bring about that m~~(x)~ IL u forxEfl ul. (4.14) (4:.! 1». Finally replacing j by p , we can arrive at a sequence ul E alfl), for which (4.13), (4.14) hold, and which are harmonic in B(E,p). Since the uj lie between fixed bounds, we conclude from the compactness property of harmonic functions (see p. 87) that there exists a subsequence of the uj(x) converging to a harmonic function W(x) for x in the compact subset B(E,p') of B(E,p). It follows from (4.13) that (s~e wf(xk)=W(x k ) for all k. (Observe that here the harmonic function W could depend on the choice of the sequence Xk and on that of the subsequence of the js.) Taking first for the Xk a sequence converging to a point x in B(E, p'), we conclude from the continuity of the corresponding W that limk~oowlxk) always exists, hence that wf is continuous in B(E,p'). Taking next for the Xk a sequence dense in B(E, p') we find that Wj agrees with a harmonic function W in all x k, and hence, by continuity, in all x E B(E, p'). This means that wf is harmonic in a neighborhood of E, and hence throughout fl. D The harmonic function wf is our candidate for the solution of the Dirichlet problem. We have to show that it has the prescribed boundary values j on afl. This requires some additional assumption on the nature of the boundary afl of fl. The assumption is formulated conveniently as existence of certain barrier junctions, that is of subharmonic functions that are zero at one boundary point and negative at all others. Barrier Postulate. Let there exist for each 7J E afl a function ("barrier function") Q'l(x) E Co(~) n a(fl), for which Q'l(7J) =0, Q'l(x)<O forxEafl,x*7J. (4.15) Lemma YD. For 7J E afl (4.16) PROOF. Let e and K be positive constants. Then u(x)= j(7J) - e+ KQ'l(x) 92 (4.17) 4 Proof of Existence of Solutions for the Dirichlet Problem belongs to CO(O)n o(~), and satisfies u(x)<f(.,,)-e forxEa~, u(.,,) = f(.,,)-e. Since f is continuous there exists a 8 = 8(e) > 0 such that f( x) >f(.,,) xEa~, Ix-.,,1<8. Then by (4.15), (4.17) f for u(x) < f(x) (4.18) for x Ea~, Ix-."I < 8. Since Q.,,(x) has a negative upper bound for Ix-."I;;> 8, we can find a K = K( e) so large that (4.18) holds as well for x E a~, Ix -.,,1;;> 8. Thus u E (10) and consequently u(x) < Wj(x) for xE~.Then also f(.,,)-e= lim u(x) <liminfw/x). x-'>." xEs:! o For e~O we obtain (4.16). Lemma vm. For." E a~ (4.19) PROOF. In view of Lemma VII it is sufficient to show that lim sup w/x) < f( .,,). (4.20) xEs:! We consider the function - W _/x) which is defined in ~ by -w_/x)= --:supu(x) foruEa_j(O). Writing u = - U we have - W_j(x)=inf U(x) (4.21) taken over all U for which -U< -f ona~. (4.22) Then for any u E 17/0) and U satisfying (4.22) u-U<O on a~, and hence in ~ by Lemma I. Thus also by (4.9), (4.21) W/x) < -w-ix) forxE~ Applying Lemma VII to W _Ix) we have then limsupw/x) <lim sup ( - W_j(x») = -liminfw_j(x) < f(.,,)· xEs:! x-'>." xEs:! x-'>." xEs:! 0 x-'>." Lemma VIII implies that wjE CO(O) when we define Wj= f on a~. We thus have proved: 93 4 The Laplace equation Theorem. If the domain !J has the postulated barrier property there exists a solution wE C 2(!J) n CO(Q) of the Dirichlet problem for arbitrary continuous boundary values f. The barrier postulate can be verified for a large class of domains !J. Take, for example, the case where the open set is strictly convex in the sense that through each p~int 1] of a!J there passes a hyperplane '1TTJ having only 1] in common with !J, We then can use for QTJ(x) a suitable linear function which vanishes on '1TTJ and is negative on Q except at the point 1]. See also the following problem. PROBLEM Show that the open set n satisfies the barrier postulate if for each 1/ E an there exists a ball B(~, p) such that 1f(~, p) and Q have just the point 1/ in common. [Hint: Use for - QTJ(x) a fundamental solution with spherical symmetry about the point ~.] 5. Solution of the Dirichlet Problem by Hilbert-Space Methods* A variety of methods have been invented to solve the Dirichlet problem for the Laplace equation. Of greatest significance are methods that make little use of special features of the Laplace equation, and can be extended to other problems and other equations. Among these is the method to be described now, reducing the Dirichlet problem to a standard problem in Hilbert space, that of finding the normal to a hyperplane. Typically the solution of the Dirichlet problem proceeds in two steps. In the first step a modified ("generalized") Dirichlet problem is solved in a deceptively simple manner. The second step consists in showing that under suitable regularity assumptions on region and data the solution of the modified problem actually is a solution of the original problem. The second step, which involves more technical difficulties, will not be carried out here in full generality. From the point of view of applications one might even take the attitude that the modified problem already adequately describes the physical situation. In this book we can only summarize the relevant properties of a Hilbert space. We start with the broader concept of a vector space S (over the real number field). This is a set of objects u, v, . " closed under the operations of addition and of multiplication with real numbers ("scalars") A, p" •••• For u,vES and scalars A,p, we have AU+p,V defined as an element of S and obeying the usual arithmetic laws. The simplest example is the set of vectors in the finite-dimensional space IRn. We next assume that in S there is defined for u, v E S a real-valued * ([9], [14], [10], [llD 94 5 Solution of the Dirichlet Problem by Hilbert-Space Methods inner product (u, v), such that (5.1) (u,v) = (v,u), (Xu + /LV, w)=X(u, w)+ /L(v, w) (0,0)=0, (5.2) (u,u»o for u'f'O, where "0" denotes both the O-element of S and the real number. (This assumption characterizes S as an "inner product space".) Property (5.2) suggests defining the length ("norm") of a vector u by lIull=Y(u,u) . One easily verifies then the Cauchy and triangle inequalities l(u,v)lo;;;;lIullllvll, A sequence limit uE S if u\u 2 , ••• lIu+vllo;;;;lIull+llvll. (5.3) (5.4) ES is said to converge to the (necessarily unique) lim lIu-ukll=O. k-4OO A sequence u \ u2 , ••• E S is called a Cauchy sequence if lim lIu k - uill =0. j,k-400 (5.5) (5.6) The space S is complete and is called a Hilbert space if every Cauchy sequence in S converges, (to an element of S). Every inner product space S can be completed, that is imbedded into a Hilbert space H in which S is dense. This completion is achieved in analogy to the construction of real numbers from rational ones. We define H as the set of Cauchy sequences {U i ,U 2 , ••• } in S, identifying Cauchy sequences {u\u 2 , ••• } and {V i ,V 2 , ••• } for which lim lIuk-vkll=O. k-4OO (5.7) We define multiplication by a scalar, addition, and inner product of elements of H by performing these operations for each element of the corresponding Cauchy sequence. It is easily seen (as for real numbers) that the resulting H is indeed complete ap.d that S is dense in H; (as a matter of fact an element of H given by the Cauchy sequence u\u 2 , ••• ES is just the limit of the Uk). A linear functional cp on an inner product space S is a real-valued function defined on S for which cp(Xu + /Lv) =XCP(u) + /LCP( v). (5.8) The functional is bounded if there exists an estimate Icp(u)lo;;;; Mllull (5.9) valid with the same M for all u E S. For any V E S the inner product (u,v)=cp(u) defines a bounded linear functional by (5.1), (5.4). In a Hilbert space H the converse holds as well: 95 4 The Laplace equation Representation theorem. Every bounded linear junctional cp on H can be represented uniquely in the form cp(u)=(u,v) with a suitable element v of H. Associating with a functional cp, (that does not vanish identically), the hyperplane 'fT in H consisting of the points u with cf>(u)= I, we can think of v as giving the direction of the normal to 'fT, since for any two points uI,u 2 in 'fT the scalar product (u I - u 2 , v) vanishes. Interpreting the direction of v as that of the normal to the plane 'fT, suggests that v also has the direction of the shortest line from the origin to 'fT. Indeed the point v v w=--=-(5.10) cp( v ) lies on 'fT, and is the point of 'fT ( v, v) closest to 0, since for any u on 'fT lIu11 2= Ilu- w+wI1 2 = IIw112+ lIu-wI1 2 +2(u-w, w) ~ IIwl12 (5.11) since (u- w,w)= (u- w,v) (v,v) cp(u)-cp(w) (v,v) O. This extremal property of w or v is made use of in the standard proof of the representation theorem. (See Problem 1.) We now reformulate the Dirichlet problem for the Laplace equation as the problem of representing a certain bounded functional cp in a Hilbert space as an inner product (u, v). In the usual version of the problem one looks for a function U with domain n satisfying Il U = 0 in 0 and U =f on ao. Assuming the prescribed f to be defined not only on ao but throughout n, we look instead for the function v = U - f for which on ao, Ilv= -w in 0 (5:12) with w=llf given. For simplicity we restrict ourselves to an open bounded connected set 0, to which the divergence theorem applies. In the space of functions of class Cl(n) we define the bilinear form (u,v) by v=O (u,v)= Jrg ~k Ux•Vx• dx. (5.13) With this definition the space C I(n) is not an inner product space, since (u,u)=O has the non-vanishing solutions u=const. Denote by ed(n) the subs.(>ace of functions u in ~ I(n) that vanish on Obviously (u, v) can be used· as inner product on by the Dirichlet integral an. cd with the corresponding squared norm given (5.14) Let v E C 2(n) be a solution of (5.12), where the prescribed w belongs to 96 5 Solution of the Dirichlet Problem by Hilbert-Space Methods CO{U). Then for any u E CJ{U) we have by the divergence theorem (u,v)= - L ullvdx= Luwdx. (5.15) This suggests that v can be found by simply representing the known linear functional cf>(u) = f uwdx (5.16) as an inner product (u,v). To make use of the representation theorem we have to complete CJ{O) into a Hilbert space HJ{O) with respect to the Dirichlet norm (5.14), and to prove that the cf>{u) defined by (5.16) gives rise to a bounded linear functional in that space. Our modified version of the Dirichlet problem is then the following: Find a v E H J{O) such that (u,v)=cf>(u) for all uEHJ(O), (5.17) where (u,v) and cf> are defined by (5.13), (5.16). To show that the functional cf> is bounded, we have to derive an inequality (5.9). Since by Cauchy (~UWdx r<L u 2 dx ~ w dx, 2 (5.18) it is sufficient to show that there exists an N such that (5.19) We show this Poincare inequality first for u E CJ{U). Since 0 is bounded it can be enclosed in a cube f: Ix;l<a fori=I,2, ... ,n. We continue u as identically zero outside O. Then for any x={x,,. .. ,xn)E f Thus 97 4 The Laplace equation Integrating over X 2 , • •• , xn from - a to a we find r r (S.19a) 2 2 2 Jr u dx <:.4a Jr uXl dx ' which implies (S.19) with N =4a 2 • An element u of HJ is represented by a Cauchy sequence U 1,U 2, ••• E CJ(Q) for which Ilu k - ujll =0. lim j.k~oo By (S.19), this implies that also r(uk-ujfdx=O. lim (S.20) j.k~oo Jo By (S.18), (S.16) the numbers </>(u k ) then form a Cauchy sequence, and we can define </> for the element u of HJ by </>( u) = lim </>( Uk). (S.21) k~oo Since also lIull = lim Ilukll k~oo by definition, the inequality (S.9) for u E CJ(Q) implies the same inequality for u E H J. One finds then that </> can be extended to the Hilbert space H J as a bounded linear functional. The representation theorem guarantees the existence of a v in HJ(U) for which (S.17) holds, and thus solves our modified Dirichlet problem. * As mentioned earlier there remains the task of identifying the solution vEHJ(U) of the modified problem with a function v that satisfies (S.12) in the ordinary sense. Here the verification of the differential equation Llv = - w, say for wEe 1(Q), is not as difficult as to show that v =0 on au. One first observes that the solution v of the modified problem is representable by a Cauchy sequence vl,v 2 , ••• in CJ(Q), with respect to the norm (S.14). This implies by (S.20) applied to the v k that v can be identified with a function which is square integrable in the sense of Lebesque in U, and for which (S.2Ia) Using for u a test function of class COO(U) and of compact support we have (v,u)= .lim (vj,u)=?-m J~OO J~OO rL v~ Jo k k Ux dx k = - .lim IvjLludx= -lvLludx. J~OO 0 0 * The modified problem can be solved more generally for any bounded open set 0 by defining HJ(O) as the completion with respect to the Dirichlet norm of the set of all u E C 2(O) that have compact support in O. This does not involve any regularity assumptions on a~. 98 5 Solution of the Dirichlet Problem by Hilbert-Space Methods Since test functions belong to Hd it follows from (S.16), (S.I7) that ! vll.udx= - ! wudx. (S.22) Hence v is a solution of the P.D.E. (S.23) ll.v= - w in the sense of distributions (see p. 69). From this we can prove that v E C2(~) and ll.v = - w. Take any z E~ and p so small that the ball B(z,3p) lies in ~. Take any test function <p with support in B(z,p) and a fixed test function r(x) which has the value I in B(z,2p). Set (S.24) where K is the fundamental solution given by (1.16). By Poisson's formula (1.28) where Thus J v(x)<p(x)dx=! v(x)<pI(x)dx+ J v(x)<p2(x)dx. (S.2Sa) Here, since r(x)u(x) again is a test function, by (S.22) J v(x)<pI(x)dx= - J w(x)nx)u(x)dx (S.2Sb) <P2(X)=ll.xJ (1- t(x»K(x, g)<p(g) dg = f. B(z,p) F(x,g)<p(g)dg. (S.2Sc) Here F(x,g)=ll.xC(I - nx»K(x,g» belongs to Coo in x,g for gEB(z,p) and all x, since K(x,g) is singular only for x =g while 1- r(x)=O in B(z,2p). Moreover Il.~F(x,g)=O, (S.26) since Il.EK(X,g) =0 for x+g. We find from (S.24), (S.2Sa,b,c) that ! v(g)<p(g)dg= J<p(g)dg(J (- w(x)t(x)K(x,g) + F(x,g)v(x»dx.) Since this identity holds for all test functions <p with support in B(z,p), we conclude that for almost all gEB(z,p) v (g) = - J K(x,g)nx)w(x)dx+ J F(x, g)v(x) dx. 99 4 The Laplace equation It follows from (5.26) and Poisson's equation (1.28) that v coincides almost everywhere* in B(z,p) with a function of class C 2 for which ~Ev(~) = - r(~)w(~) = - w(~). Since z is arbitrary we have ~v = - w throughout n. The proof that v has boundary values 0 will be given here only for the dimension n=2. Prescribe a number e>O. To v there corresponds a Cauchy sequence v k E We can find a number j such that eden). Ilvj-vkll,e e for all k>j. Denote by d(~ for ~En the distance of ~ to a closest point of the boundary curve an. We assume that an is sufficiently regular and d(~)=I~*-~1 sufficiently small. Then each x in B(~,d(~) can be joined to a point of an by a segment parallel to ~~* and of length '4dm. The union U of these segments covers B(~,d(~» (See Figure 4.3). Poincare's inequality (5.19a) applies* to u=Vj-V k in U and yields that f f (v j - Vk)2dxl dX2' 16d2(~)lIvi _v k Il 2 , 16d2(~)e2 u for k >j. By (5.21a) then f f (vi - V)2 dx 1 dx 2, 16d2(~)e2. (5.27) B(E,d(~) For the solution v of ~v = - w we have by (1.24) v(~)= - f f (1f(lx-~I)-1f(p»W(X)dXldx2+-21 ~~ r ~~~~ v{x)ds, (5.28) where.1f(p)=(1/2'1T)logp. Let M=maXnlwl. Multiplying (5.28) by p and integrating with respect to p from 0 to d(~ we find that '1Td2{~)lv{~)I' f f Ivldx+O(M d 4m) B(E,d(~) , f f Iv-vjldx+ B(E,d(~» ff Ivjldx+O(Md4{~». B(~,d(m Since the continuous function vi vanishes on an we have Ivi(x)1 < e for x E B(~,d(~) provided dm is sufficiently small. In addition by (5.27) ( flv-dl dX)2 ''1Td 2{O B(E,dm) f f (v-vjidx'16'1Td4{~)e2. B(~,d(~» • As a distribution the values of v are only determined "almost everywhere." tIn the proof of (S.l9a) we did not need that u vanishes everywhere on the boundary of n. It is sufficient to know that in n each coordinate has a range of length .;;; 2a, and that each point of n can be joined in n by a parallel to the XI-axis to a point where u vanishes. 100 5 Solution of the Dirichlet Problem by Hilbert-Space Methods Figure 4.3 It follows then that for sufficiently small d(~ v(~) =O(e+ M d2(~)). This implies that v(~) tends to 0 as ~ approaches the boundary a~. PROBLEMS 1. Prove the representation theorem in Hilbert space H by finding a point in a plane with the minimum distance from the origin. [Hint: Let m=infllull for q,(u)= 1. Take a minimizing sequence w k with </>(w k) = 1, IIwkll~m. From k m2~11 w ;w' r=-}lIwkIl2+-}1I~1I2-illwk-~112 . prove that the w k form a Cauchy sequence converging to an element w of H with q,(w)= 1, IIwll = m. Show that (w,u)=O for q,(u)=O, and finally that (v,u)=q,(u) for v=w/(w,w) and all u.J 101 4 The Laplace equation 2. Show that a solution U E C 2(n) of ~U=O inn, U=J onan minimizes the Dirichlet integral (U, U) among all functions in C 1(fi) with boundary values J ("Dirichlet's principle"). Show that the corresponding modified Dirichlet problem consists in finding a v satisfying (5.17) for the functional q,(u) =(u,f). 3. Consider the Dirichlet problem for n = 2 with n being the unit disk referred to polar coordinates r,O. Let J(O) denote the boundary values assumed to be continuous, and u(rcosO, rsinO) the solution of ~u=O with boundary valuesJ, known to be of class C 2(n) n Co(n). (a) Show that for r< 1 00 u= ~ (akcoskO+bksinkO)rk, k=O (5.29) where ak,bk are the Fourier coefficients of J. [Hint: prove first that u has a Fourier expansion of the form (5.29) for r< I with certain anobn • Show that by continuity the anobn are the coefficients of J.] (b) Show that the Dirichlet integral of u is given by (5.30) (c) Show that there are continuous J for which the Dirichlet integral for the corresponding u is infinite. [Hint: Find sequences ak, bk for which the series in (5.30) diverges, while the series 00 ~ (Iakl + Ibkl) k=\ converges.] (This shows that the Dirichlet problem cannot be solved for all continuous boundary values by the Hilbert-space approach.) 4. (Best constant 1fA in Poincare's inequality). Show that if there exists a function u E C 2(n) vanishing on an for which the quotient (u,u) fDf u dx 2 reaches its smallest value A, the~ u is an eigenfunction to the eigenvalue A, so that ~U+AU=O in n. In fact A must be the smallest eigenvalue belonging to an eigenfunction in C 2(n). 102 Hyperbolic equations in higher dimensions* 5 1. The Wave Equation in n-dimensional Spacet (a) The method of spherical means The wave equation for a function u(x\, ... ,xn,t)= u(x,t) of n space variables X\""'Xn and the time t is given by Ou=Utt -C2AU=0 (1.1) with a positive constant c. The operator "0" defined by (1.1) is known as the D' Alembertian. For n = 3 the equation can represent waves in acoustics or optics, for n = 2 waves on the surface of water, for n = 1 sound waves in pipes or vibrations of strings. In the initial-value problem we ask for a solution of (1.1) defined in the (n + I)-dimensional half space t > 0 for which u= f(x), ut=g(x) for t=O. (1.2) The initial-value problem (1.1), (1.2) can be solved by the method of spherical means due to Poisson. We associate generally with a continuous function h(x)=h(x\, ... ,xn) in IR n its average Mh(x,r) on a sphere with center x and radius r: (1.3) Setting y = x + r~ with I~I = 1, we get Mh(x,r)=-.!.. ( Wn J1g1 = I h(x+r~)dS~. (1.4) *([15]. [19D t([2]. [6]. [17D 103 5 Hyperbolic equations in higher dimensions Originally Mh(x,r) is defined by (1.3) only for r>O. We can extend its definition to all real r using (1.4). The resulting Mh(x,r) then is an even function of r, since replacing r by - r in (1.4) can be compensated for by replacing the variable of integration ~ by -~. It is also clear from (1.4) that Mh E C S (Rn+ 1) for h E C S (Rn) since we can differentiate under the integral sign. For h E c 2(Rn) we find from (1.4), using the divergence theorem (4.1) of Chapter 3 that a I -ar Mh(x,r)= -wn )Ilil r = 1 i~= 1 hx;(x+r~)~idSIi n =~ Wn r )11;1<1 axh(x+r~)d~ MUltiplying by r n - I and differentiating with respect to r yields ;r(r n- I ;rMh(x,r»)=axrn-IMh(x,r). (1.5) Thus the spherical means Mh(x,r) of any function hE c 2(Rn) satisfy the partial differential equation a) Mh (x,r) =axMh(x,r) ( ara + -n-I - -a r r 2 -2 (1.6) known as Darboux's equation. Using that the solution Mh(x,r) of (1.6) is even in r, we find for its initial values ( aa Mh(x,r») Mh (x,O)=h(x), r r=O =0. (1.7) Forming spherical means we can transform the initial-value problem for the wave equation into one for a hyperbolic equation in two independent variables. Let u(x,t) be a solution of (1.1), (1.2) of class C 2 in the half space x ERn, t > O. We form the spherical means of u as a function of x: Mu(x,r,t)= ~ Wn r )1~1=1 u(x+r~,t)dSIi. (1.8) Obviously u can be recovered from M u , since Mu(x,O,t) = u(x,t). 104 (1.9) 1 The Wave Equation in n-dimensional Space By (1.6) !1xMu = a) Mu' ( ara2 + -n-l - -a r r -2 On the other hand by (1.1), (1.8) !1xMu=~ Wn r JI~I= I !1xu(x+r~,t)dS~ 1 a -1 =2"-2 2 c at Wn i a2 1~1=1 1 u(x+r~, t)dS~=2"-2Mu' c at Hence Mu(x,r,t) as a function of the two scalar variables r,t for fixed x is a solution of the P.D.E.* (1.10) The P.D.E. (1.10) depending on the parameter n (here equal to the dimension of x-space) is known as the Euler-Poisson-Darboux equation. Our Mu as function of r,t by (1.2), (1.8) is a solution of (1.10) with the known initial values (1.11 ) The initial-value problem (1.10), (1.11) can be solved most easily when the number of space dimensions is n = 3t Indeed by (1.1 0) (1.12) Thus rMu(x,r,t) as a function of r,t is a solution of the one-dimensional wave equation with initial values (1.13) • The expression 02 n-l 0 -+--or2 r or has been encountered already (Chapter 4, (1.9)) as the Laplacian of a function in R" depending only on the distance r from a fixed point. Equation (1.10) thus asserts that the spherical means of a solution of (1.1) on spheres with center x again form a solution of (1.1). This is to be expected since the spherical means could plausibly be obtained by rotating the solution u in all possible ways about x and averaging over all rotations. Since the wave equation is invariant under rotations this procedure should lead again to a solution. tThis is more difficult for other values of n. See problem 2. 105 5 Hyperbolic equations in higher dimensions Thus by our general formula «4.13) of Chapter 2) rMu(x,r,t) = "2I [(r+ct)Mix,r+ct)+(r-ct)Mix,r-ct)] Using that MtCx,r) and Mg(x,r) are even in r we are led to Mu(x,r,t) = (ct + r)Mix,ct+ r) - (ct - r)Mix,ct- r) 2r I + -2 f ct + r ~Mg(x,~)d~. rc ct-r Letting r tend to 0 and replacing differentiation with respect to r by differentiation with respect to ct, we find by (1.9) that u(x,t)= tMg(x,ct) + :t (tMix,ct») = ~I g(y)dSy+ .l.(~I 4'1TC t Iy-xl=ct at 4'1TC t Iy-xl=ct f(Y)dSy ). (1.14) Any solution u of the initial-value problem (1.1), (1.2) of class C 2 for t>O in n=3 space dimensions is given by formula (1.14), hence is unique. Conversely for any f E C3(~3) and g E C2(~3) the u(x, t) defined by (1.14) is of class C 2 and satisfies (1.1), (1.2). Indeed (1.2) follows by inspection, using (1.7). Moreover by (1.6) for n=3 and r=ct a2 a2 - (tMg (x,ct») = c -2 (rMg (x,r») = cr!l.xMg (x,r) = c 2!l.A tMg (x, ct». at 2 ar Thus tMg(x,ct), and similarly (a/at)tMj(x,cO, satisfy the wave equation (1.1)* . Formula (1.14) displays the relevant features of the solution u of the initial-value problem for the wave equation in the case n = 3. First of all, writing our spherical means in the form (1.4). we can carry out the I-differentiations under the integral sign, arriving at the expression U(X,t)=~f 4'1TC t (tg(y)+f(y) + Iy-xl=ct ~.iy.(y)(yj-X;))dSy. i • (1.15) (1.15) indicates that u can be less regular than the initial data. There is a possible loss of one order of differentiability: u E e, Ut E C s + 1 initially, guarantee only that u E c s - 1, ut E C S at a later time. This is the focussing effect, present when n> 1t. For example the second derivatives of u could . . ·Incidentally the first expression for u in (1.14) defines u as a solution of (l.l) for all x,t, since Mj(x,ct), Mg(x,ct) are defined for all t as even functions in t. t Irregularities in the initial data are "focussed" from different localities into a smaller set, ("caustic") leading to stronger irregularities. This phenomenon does.not occur for n= I where u is no worse than its data, as shown by formula (4.13) of Chapter 2. 106 1 The Wave Equation in n-dimensional Space become infinite at some point for t > 0, though they are bounded for t = o. In contrast to the pointwise behavior of u, we shall find that in the L2-sense U does not deteriorate. This follows from the fact that the energy norm of U E(t)=i J J J(ut(X,t)+C2~U;i(X,t))dX (1.16) does not change at all with t. Indeed c;: = J ( UtUtt + c2 ~ Ux,Uxit ) dx = J =0 ( utDu + c 2 ~ (UtUx,) Xi) dx (1.16a) if u(x,t)=O for all sufficiently large IxiAccording to (1.15) the value u(x,t) depends on the values of g and ofJ and its first derivatives on the sphere S(x,ct) of center x and radius ct. Thus the domain oj dependence for u(x,t) is the surface S(x,ct). (See Figure 5.1.) Conversely the initial dataJ,g near a pointy in the plane t=O only influence u at the time t in points (x, t) near the cone Ix - yl = ct. (See Figure 5.2.) Let J,g have their support in a set U E 1R3. In order that u(x, t)+O the point x has to lie on a sphere of radius ct with its center y in U. The union of all spheres S(y,ct) for y EU contains the support of u at the time t. This gives rise again to Huygens's construction for a disturbance confined originally to U. (See· p. 30.) The support of u spreads With velocity c. It is contained in the region bounded by the envelope of the spheres of radius ct with centers on au. Actually the support of u(x, t) can be smaller. Take, for example, for the region U containing the support ofJ,g the ball B(O,p) of radius p and center o. Then S(x,ct) for ct>p will have a point in common with U only when x lies in the spherical shell bounded by the spheres S(O,ct+p) and S(O,ct-p). For any fixed x and all sufficiently large t (namely t> (lxl + p)/ c) we have u(x, t) =0. A disturbance originating in B (0, p-) is confined at the time t to a shell of Figure 5.1 107 5 Hyperbolic equations in higher dimensions ~ ~ I t=O Figure 5.2 u=O t =0 Figure 5.3 thickness 2p expanding with velocity c. (See Figure 5.3.) This accounts for the .possibility of "sharp" signals being transmitted in accordance with equation (1.1) in three dimensions. This phenomenon is due to the fact that the domain of dependence for u(x,t) is a surface in x-space rather than a solid region ("Huygens's principle in the strong form"). For most hyperbolic equations (even for the wave equation in an even number of dimensions) the principle does not hold. Disturbances propagate with finite 108 1 The Wave Equation in n-dimensional Space speed but after having reached a point never die out completely in a finite time at that point, like the surface waves arising from a stone dropped into water. While the support of the solution with initial data of compact support expands, the solution decays in time.* Assume that j,g and the first derivatives of j are bounded, and vanish outside B(O,p). Contributions to the integral in (1.15) arise only from that portion of the sphere S(x,ct) that lies inside the ball B(x,p). Elementary geometry shows that the area of intersection of any sphere in 3-space with a ball of radius p is at most 4'1Tp2. Thus the integral is at most equal to the maximum of the absolute value of the integrand multiplied by 4'1Tp2. It follows that u for large t is at most of the order of 1/ t. PROBLEMS 1. (a) Show that for n=3 the general solution of (1.1) with spherical symmetry about the origin has the form F(r+ct)+ G(r-ct) u=------r r=lxl (1.17) with suitable F, G. (b) Show that the solution with initial data of the form u=O, ut=g(r) (1.18) (g=even function of r) is given by 1 u= -2 cr i r + ct pg(p)dp. (1.19) for O<r<a for r>a (1.20) r-ct (c) For g(r)= {~ find u explicitly from (1.19) in the different regions bounded by the cones r=a±ct in xt-space. Show that u is discontinuous at (O,a/c); (due to focussing of the discontinuity of Ut at t=O, Ixl=a). 2. Consider the initial-value problem (1.1), (1.2) for the wave equation in n=5 dimensions. With Mu(x,r,t) defined by (1.8), set N (x,r,t)= r2 :r Mu (x,r,t) +3rMu (x,r,t). (1.21) (a) Show that N(x,r,t) is a solution of a 2-aN -N=c at 2 ar2 and find N from its initial data in terms of M j and Mg. 2 * For the analogous 2 situation of surface waves in water (n=2) compare Shakespeare (Henry VI,part I): Glory is like a circle in the water Which never ceaseth to enlarge itself Till by broad spreading it disperse to nought. 109 5 Hyperbolic equations in higher dimensions (b) Show that . N(x,r,t) u(x,t)=lim 3 r .....O r 3. For X= (Xh X2,X3) consider the equation of elastic waves (see (2.8) of Chapter 1) LU=(~ -cr~)(~ -d~)U(X,t)=O at 2 at 2 (1.23) with positive distinct constants Ch C2. (a) Show that Mu(x, r, t) defined by (1.8) satisfies ArM =(~-cr~)(~-ci~)rM =0. u at2 ar2 at2 ar2 u (b) Show that the general solution v(r,t) of Av=O is of the form v= FI (r+ clt)+ F2(r- clt)+ G I (r+ C2t) + G2(r- c2t). (c) Solve the general initial-value problem for (1.23) using (a) and (b). (b) Hadamard's method of descent In this method solutions of a partial differential equation are obtained by considering them as special solutions of another equation which involves more independent variables, and can be solved. For example a solution U(x\,X2,t) of (1.1), (1.2) with n=2, can be looked at as a solution of the same problem with n = 3 which happens not to depend on X3. Then U(X\,X2,t) is given by formula (1.14) for x 3=0 with g(y) = g(y\,Y2), f(y) = f(y\,Y2), the surface integrals being extended over the sphere Iy - xl =V(y\-x\?+(Y2-X2)2+y~ Observing that on that sphere 110 =ct. 1 The Wave Equation in n-dimensional Space where r=y(x l -yl+(X2-Y2i (1.24b) We observe that here the domain of dependence of the point (XI,X2,t) on the initial data consists of the solid disk r<. cl in the YIY2-plane. Thus Huygens's principle in the strong form does not hold for the wave equation in two dimensions. Disturbances will continue indefinitely, as exhibited by water waves. The same method can be applied to other lower-dimensional equations as well. Consider, for example, a solution u of (1.1), (1.2) with n = 3 of the special form U(X I,X2,X3' I) = eiAx3v(xI,X2' I). Then v is a solution of the 2-dimensional equation (1.25) The solution v of (1.25) with initial values vt =I/I(X I,X2) for 1=0 V = </>(X I,X2), (1.26) is obtained from formula (1.14) for X3 =0, taking PROBLEMS 1. Write out the solution of the initial-value problem (1.25), (1.26). 2. Show that the solution w(x), t) of the initial-value problem for the telegraph equation (1.27) (1.28) is given by (1.29) Here s= C2r 2 -(XI-y)2 (1.30) while J o denotes the Bessel function defined by Jo(z) = ~ ('1T/2cos(zsinfJ)dfJ. 'lI' Jo (1.31) [Hint: "Descend" to (1.27) from the two-dimensional wave equation satisfied by U(X),X2, t) = COS(Ax2)W(X), t). Use formulas (1.24a, b).] 111 5 Hyperbolic equations in higher dimensions 3. Solve the initial-value problem (1.1), (1.2) for n=4 by descent from the solution (1.22) for n = 5. (C) Duhamel's principle and the general Cauchy problem Consider the inhomogeneous wave equation Du(x,t)=w(x,t) (1.32) for a function u(x,t) with initial values u(x,O)= f(x), ut(x,O)=g(x). (1.33) Duhamel's principle permits reduction of the problem (1.32), (1.33) to a succession of problems of the type (1.1), (1.2) for the homogeneous wave equation. (The method, the analogue of the method of "variation of parameters" for ordinary differential equations, applies to more general linear partial equations.) It is sufficient to consider the problem (1.32), (1.33) for the special case where the initial data are u(x,O)=ut(x,O)=O. (1.34) We only have to subtract from U the solution of the problem (1.1), (1.2) which we assume to be known. We claim that the solution of (1.32), (1.34) is given by u(x,t)= fotU(x,t,s)ds, (1.35) where U(x, t,s) for each fixed s >0 is the solution of DU(x,t,s)=O fort>s (1.36) with initial data prescribed on the plane t = s: (1.37) Ut (x,s,s)= w(x,s). Let indeed U(x,t,s) be a solution of (1.36), (1.37) of class C 2 in its arguments for x ERn, 0.;;;; s';;;; t. Then for the u given by (1.35) U(x,s,s)=O, ut = U(x,t,t)+ fot Ut (x,t,s)ds = fotUt(x,t,s)ds utt = (1.38) ~(x,t,t)+ fot~t(x,t,s)ds = w(x,t) + fotc2Llx U(x, t,s)ds = w(x,t) + c 2Llxu(x,t), confirming (1.32). That U satisfies the initial conditions (1.34) is clear from (1.35), (1.38). Since the wave operator 0 is invariant under translations, we have in V(x,t,s)= U(x,t+s,s) (1.39a) a solution of the wave equation DV(x,t,s)=O 112 fort>O (1.39b) 1 The Wave Equation in n-dimensional Space with initial values prescribed for 1=0: V(x,O,s)=O, ~(x,O,s)=w(x,s). (1.39c) For n = 3 formula (1.14) yields in V(x,l,s)= ~I w(y,s)dSy 4'1TC t Iy-xl=ct a C 2-solution of (1.39b, c) provided w(x, I) E C 2 for I;> 0 and all x. Substituting into (1.35) leads to the expression U(X,/)= fotV(X,I-S,s)ds = ~ rt ~I 4'1TC )0 I-s Iy-xl=c(t-s) w(y,s)dSy • (1.40) Thus the value of the solution u of (1.32), (1.34) at the point (x, I) depends only on the values of w in points (y,s) with ly-xl=c(/-s), O<s<t, (1.41) that is, on the values of w in points of the upper half space lying on the backward characteristic cone with vertex (x, I). This truncated cone represents the domain of dependence of u(x, I) on w. The Cauchy problem for (1.32) (and similarly for other equations) with an arbitrary initial surface S in xl-space can be reduced to that for t=O. Let the hypersurface S be given by I = </>(x) =</>(X\,X2,X3)' We prescribe Cauchy data u= f(x), (1.42) ut=g(x) for (x,/) on S. Of course, S will have to be noncharacteristic, that is, \fI(x) = 1- c2~ </>x,';60 (1.43) (1.44) i (see (2.28a, b) of Chapter 3). To simplify the expression we make the (unessential) assumption that </>,j,gEc oo (1R3), WEc oo (1R4), and that </»0. To find a solution u of Du(x,/)=w(x,/) for I > </>(x) (1.45) with Cauchy data (1.43), we first construct an approximale solulion v of order 2, i.e., a function v(x, I) which just on S satisfies v=f, a a2 Dv-w= -(Dv-w)= -(Dv-w)=O. (1.46) al a/2 We can always find a special v satisfying (1.46) in the form of a 4th-degree polynomial in I: 4 v(x,/)= L ai(x)(/-</>(x»)i (1.47) i=O 113 5 Hyperbolic equations in higher dimensions (this is just the beginning of the formal Cauchy-Kowalewski expansion for u in terms of powers of t-q,). The coefficients aj(x) have to be found recursively from ao=j, al=g 21/1a2 + c2(~(alq,- ao) -q,~al) = w(x,q,) 61/1a3+ c2(~(2a2q,- a l ) 2q,~a2) = wt(x,q,) - 241/1a4 + c2(~(6a3q,- 2a2) - 6q,~a3) = wtt(x,q,). (1.48a) (1.48b) (1.48c) (1.48d) The aj exist because of (1.44). We change our problem (1.45), (1.43) to one for the function U = u - v. We then want OU(x,t)= W(x,t) for t>q,(x) U= Ur=O for t=q,(x). (1.49a) (1.49b) Here W(x,t)=W(x,t)-Ov(x,t) (1.50) belongs to C OO(1R4) and, by (1.46), satisfies W(x,t)= W,(x,t)= w,t(x,t)=O for t=q,(x). (1.51) Then all first and second derivatives of W vanish for t=!f>(x) and the function W* defined by W(x,t) W* ( x t ) = ( , 0 for t>q,(x) fort<;q,(x) (1.52) belongs to C 2(1R4). We replace the Cauchy problem (1.49a, b) by the initial-value problem OU(x,t)= W*(x,t) for t>O U(x,O)= Ur(x,O)=O (1.53a) (1.53b) for which we can find a solution of class C 2 for t > 0 with the help of formula (l.40). We claim that the U found from (1.53a, b) satisfies (1.49a: b) provided S is spacelike in the sense that 1/1 (x) = 1- c 2 ~ q,:,> O. (1.54) j Clearly (1.53a) implies (1.49a), since q,>0. Moreover, (1.49b) follows if we show that U(x,t)=O for t<q,(x). Now by (l.40) U(x,t)=O if W*(y,s)=O in all points of the backward characteristic cone (see Figure 5.4) Ix-yl<c(t-s), O<s<t (1.55) with vertex (x,t). By (1.52) this will be the case if we can show that s<q,(y) whenever (1.55) holds and t<q,(x). Now s>q,(y) would imply 114 1 The Wave Equation in n-dimensional Space s t = rj>(x) t=O Figure 5.4 that Ix-yl..;: c(t- s) < c{cp(x) -cp(y)) = c ~ cpx,(n(xj-Yj) j <'Y~ cp~(~) Ix-yl with an intermediate point r Using (1.54) this leads to a contradiction, and (1.49b) is established. In this way the existence of a solution of the Cauchy problem with data on a spacelike surface S is established. The argument will not work if S is not spacelike, since then the cone (1.55) might contain points where W*~O. Data on "timelike" surfaces with l/I(x)<O or surfaces which are partly spacelike and partly timelike cannot be prescribed arbitrarily, since then some points of S lie in the domain of influence of others. Uniqueness for the Cauchy problem (1.45), (1.43) is trivial. Let u be a solution with homogeneous dataf=g=w=O and of class C 2 for t~cp(x). We can then continue u as identically 0 to all (x,t) with 0<. t<cp(x). Then u becomes a C 2-solution of Du = 0 with vanishing initial data for t = 0, and hence vanishes identically. 115 PROBLEM Let S denote a spacelike hyperplane with equation t=yx, in xt-space. Show that the Cauchy problem for Du = 0 with data on S can be reduced to the initial-value problem for the same equation by introducing new independent variables x',t' by the Lorentz transformation (d) Initial-boundary-value problems ("Mixed" problems) So far we have considered the "pure" initial-value problem for the wave equation, with x ranging over the whole space ~n for t>O. We next consider solutions u(x, t) of for xEn, t>O, Du=w(x,t) (1.56) where n is an open set in x-space. For simplicity we take n=3. We associate with the operator 0 the energy integral E(t)= l!( Ul+C2~ U~)dx o (1.57) I (see (1.16)*). Then, using (1.56) ~= = = l( 1(C2~ o o UtUtt + c 2 ~ UxYx,t) dx I (utux)x, +UtW)dx I rutwdx+ J(aoc2utddun dSx' )0 (1.58) where d / dn denotes differentiation in the direction of the exterior normal to an. If here U= ut=O for xEn, t=O u=O or du/dn=O for xEan, t>O Du=O for xEn, t>O (1.59a) (1.59b) (1.59c) it follows that E(t)=O for t>O, since E(O) =0, dE/dt=O. Since the integrand in (1.57) is a definite quadratic form in the first derivatives of u, we conclude that ut = ux . = 0 for x En, t > 0, hence that U is constant, and thus u=O because u=O initially. Consequently (subject to appropriate regularity assumptions) a solution u of (1.56) is determined uniquely given * In many applications E 116 represents the sum of kinetic and potential energy. 1 The Wave Equation in n-dimensional Space (a) the values of w for xEQ, t>O, (b) initial values u=f(x), ut=g(x) forxEQ,t=O, (1.60) and (c) boundary values ("Dirichlet data") for xE aQ, t>O u=h (1.61) (where instead of u, du / dn can also be prescribed on aQ). In the special case where w = h = 0, the solution can be found by expansion into eigenfunctions for the Laplace operator for the region Q, in analogy to (4.21) of Chapter 2. An eigenfunction v(x) corresponding to the eigenvalue A is a solution of dV(X)+AV(X)=O for xEQ (1.62a) v (x) = 0 for x E aQ, (1.62b) where v does not vanish identically. Under appropriate regularity assumptions on Q there exists a sequence of eigenvalues Ak and a corresponding sequence of eigenfunctions vk(x) which form a complete orthonormal set on n. (See Courant-Hilbert [7].) This leads to an expansion u(x,t)= ~ak(t)vk(t) (1.63) k for the solution u(x, t) of our initial-value problem. Substituting into the equation u=O and comparing coefficients, one finds that the ak(t) are solutions of the ordinary differential equation ak(t)+c2~ak(t)=0. (1.64) Using the initial conditions (1.60) and Fourier's formula ak = k UVk dx (1.65) for the coefficients of an expansion in terms of orthonormal functions, one arrives at initial conditions (1.66) Equations (1.64), (1.66) easily permit us to determine the ak(t) as trigonometric functions of t: a,(t)- [ [ J(X)COs(cl.,t) + g(X):~cl.,t) ]V,(X)dx. (1.67) Some mixed problems can be solved "in closed form" when the space region Q is the halfspace Xn > O. The principal tool here is the extension to the whole space by reflection. Let u be the solution of Du= w(x,t) u=f(x), for X3 >0, t >0 (1.68a) ut=g(x) (1.68b) U=h(XI,X2,t) forx3>0,t=0 for X3=0, t>O. (1.68c) 117 5 Hyperbolic equations in higher dimensions Relations (1.68a, b, c) imply certain consistency conditions between the data j,g,h, W, at least if a solution u of class C 3 is to exist in the closed quadrant X3~0, t~O: j=h, c 2/lg + W t = hili g=h" for X3 = t = O. (1.69) We shall construct a solution u of class C 2 for X3 ~ 0, t ~ 0, provided the dataj,g,h, w, have sufficiently many derivatives in their domains of definition and satisfy (1.69). Moreover the solution is unique. For that purpose we first simplify the problem by making use of an approximate solution v(x,t) oj order 2 of (1.68a, b) (see p. 113), that is, a solution of Oi - . (Ov- w)=O for i=O, 1,2 when x 3=0, t ~O. (1.70) v=h, OX3 We can always find such a v that is a polynomial in X3 4 V=h(Xl,X2,t)+ ~ ai(Xl,x2,t)X~ (1.71) i=2 with suitable coefficients a2,a3,a4' It remains to find a solution U(x,t)= u(x,t)-v(x,t) of oU= W= W - Ov for X3 ~ 0, t ~ 0 U= F(x) = j(x) - v(x,O), Ut = G (x) = g(x) -vt(x,O) for X3 ~ 0, t=O U=H=O for x 3=0, (1.72a) t~O. (1.72b) (1.72c) Observe that here by (1.70), (1.69) W = WXjX3 = 0 for X3 = 0, t ~ 0 F=FX3X3 =G=GX3X 3 =0 forx3=0. (1.73a) (1.73b) If we extend F, G, W by "reflection" to all values of X3' so as to be odd in X3' then the resulting functions F*, G*, W* will be defined for all x. Moreover by (1.73a, b) F* E C 3 , G* E C 2 for all x, and W* E C 2 for all x and t ~ O. We can then solve the pure initial-value problem U= W* U=F*, for t>O (fr= G* for t=O using formula (1.40) to obtain a C 2-solution. Obviously the restriction of U to values X3 ~ 0, t ~ 0 satisfies (1.72a, b). Moreover U is odd in x 3, since U(Xl,X2,X3,t)+ U(Xl,X2' - X3,t) 118 I The Wave Equation in n-dimensional Space will be a solution of the wave equation with initial values 0, thus vanish identically. This also implies that (1.72c) holds. Finally a C 2-solution u of (1.68a, b, c) is unique. Since for j=g=h=w=O it could be extended by reflection to a solution of the wave equation with initial values that are 0 everywhere, and hence would vanish. We observe that the consistency conditions (1.69) are satisfied automatically, when h =0 and in addition j,g, w vanish for all sufficiently small x 3• PROBLEMS 1. Let n denote an open bounded set in n-dimensional x-space described by an inequality ![>(x) >0, so that q,(x)=O on an. Let SA for A;;;' 0 denote the hypersurface in xt-space given by t=Aq,(X) for x En. On SA define for a function u(x,t) the energy integral E(A)= where QA = i (u? + c2 1. QA dx, (1.74a) s~ ~ U;' ) + Ac2ut ~ UXiq,x/ (1.74b) (a) Prove E(A)=const. when Ou=O. [Hint: Integrate utOu over the lens-shaped region O<t<Aq,(X).] (b) Show that QA as a quadratic form in u"ux" ... ,uxn is positive definite, when SA is spacelike. (c) Show that the initial data on So of a solution of Ou=O uniquely determine u on all SA with sufficiently small A. (Compare Holmgren's theorem, p. 66.) 2. Let u be a solution of (1.68a, b, c) where f = h = w = O. Find the domain of dependence of u(x,t) on g. 3. Consider the mixed problem for u(x,t)=U(XI>X2,x3,t) (1.75a) Ou=O for X3 >0, t>O u=f(x), u,=g(x) forx3>0,t=0 Mu=O for X3=0, t>O, (1.75b) (1.75c) where M denotes a first-order operator of the form (1.75d) with constant coefficients a;, and f,g vanish for all sufficiently small X3 >0. Prove there exists a solution u provided a3";; O. (Compare problem 2, p. 43.) [Hint: First determine v = Mu for X3 > 0, t > 0 from its initial and boundary conditions as a solution of Ov = O. Next find u for X3 > 0, t > 0 as a solution of Mu = v with initial condition u = f by the methods of Chapter 1. Verify that the u obtained satisfies (1.75a, b, c).] 119 2. Higher-order Hyperbolic Equations with Constant Coefficients (a) Standard form of the initial-value problem For functions u(x,t)= U(XI, ... ,Xn,t) we define the differentiation operators D=(DI, ... ,Dn)=( a: a: 1 , ... , n )' r= :t (2.1) where D is the gradient vector with respect to the space variables. Using the Schwartz notation of Chapter 3 we can write the most general mthorder linear partial differential equation with constant coefficients in the form (2.2) P(D,r)u=w(x,t), where P(D,r)=P(DI, ... ,Dn,r) is a polynomial of degree m in its n+ 1 arguments. We associate with equation (2.2) in the half space t>O the initial conditions rku =lk(x) fork=O, ... ,m-l andt=O. (2.3) We shall assume that the plane t=O is noncharacteristic. This means that the coefficient P(O, 1) of rm in the polynomial P does not vanish. Dividing by a suitable constant we can bring about that P(O,I)=l. (2.4) Problem (2.2), (2.3) for general data W,jk can be reduced to the standard problem where the data have the special form w=10= II = ... =Im-2=0, 1m-I =g(x). (2.5) The solution of the standard problem (unique by Holmgren's theorem) will be denoted by ug(x, t). To achieve this reduction we first find a solution u of (2.2) with zero initial data. Such a solution is furnished according to Duhamel's principle by the formula u(x,t)= fotU(x,t,s)ds, (2.6) where U (x, t, s) for each parameter value s > 0 is the solution of the initial-value problem P(D,r)U(x,t,s)=O fort;;;.s rkU(x,t,s)=O for k=0, ... ,m-2 and t=s rm-IU(x,t,s)= w(x,s) for t=s. (2.7a) (2.7b) (2.7c) That it solves (2.2) is easily verified, using (2.4). Here for each s ;;;. 0 the 120 2 Higher-order Hyperbolic Equations with Constant Coefficients function U(x,t,s) is found by solving a standard problem; in fact U(x,t,s)=ug(x,t-s) where g(x)=w(x,s). (2.8) It remains to reduce the solution of the homogeneous equation P(D,T)U=O (2.9) with general initial conditions (2.3) to standard problems. For that purpose we arrange the polynomial P(D,T) according to powers of T: P(D,T)=Tm+PI(D)T m- I+ ... +Pm(D), (2.10) where Pk(D) is a polynomial of degree <.. k in DI, ... ,Dn. Using the differential equation (2.9) one easily verifies that the solution U with initial data (2.3) is representable in terms of the standard problems associated with each individual A by the formula u= ufm_l +( T+ PI (D »)ufm_2 +( T2+ PI (D )T+ PiD »)ufm _3 + ... +(Tm-I+PI(D)Tm-2+PiD)Tm-3+ ... +Pm-I(D»ufo . (2.11) As an example we have for the solution of the wave equation (T2 - c2,:l)u = 0 with initial values U=j, u/=g fort=O the formula in agreement with (1.14). A system of N linear partial differential equations of order m for N functions UI, ... , UN can also be written in the form (2.2), where now U stands for the column vector with components UI' ... 'UN, and P(D,T) is a square N X N matrix whose elements are polynomials of degree <.. m in DI, ... ,Dn,T. The data w,A in (2.2), (2.3) are column vectors. The solution ug of a standard problem corresponds to the data (2.5). For a noncharacteristic initial plane t = 0 the matrix P (0, I) is nondegenerate, and we can assume that P(O,I)=1 (2.12) is the unit matrix. The solution of (2.2) with zero initial data still is described by Duhamel's formulas (2.6), (2.7a, b, c), and thus reduced to standard problems as in (2.8). The reduction of general initial data to standard ones is achieved by a modification of (2.11) which reads m-2up .+ ... +up .). u=uj,m-i + (TUj,m-2 +uPj, )+ ... +(T m- IU.+T I m-2 JO )JO m-lJO (2.13) 121 5 Hyperbolic equations in higher dimensions In what follows we shall only have to deal with the standard problem P(D,r)u=O 'l"ku=O fort::>O for k=0, ... ,m-2 and t=O 'l"m-lu=g(x) for t=O. (2.14a) (2.14b) (2.14c) We call the differential equation or system of equations (2.14a) hyperbolic (with respect to the plane t=O), if the initial-value problem (2.14a, b, c) has a solution u(x,t) of class em, for all g(x) E CO (Rn), where s is sufficiently large. * We also say that the plane t = 0 is spacelike. PROBLEM Verify that formulas (2.11), respectively (2.13), give the solution of the initial-value problem (2.3), (2.9). (b) Solution by Fourier transformation Following Cauchy a formal solution of the standard problem (2.14a, b, c) can be obtained by Fourier transformation with respect to the space variables. It will be an actual solution if the integrals involved converge adequately. We associate with a function g(x)E CO (Rn) its Fourier transform g, defined by (2.15) (x·~= Xl~l + ... formula + xn~n).t For g E CO with sufficiently large s the reciprocal (2.16) holds. We find from (2.15) by integration by parts for any k=I,2, ... ,n that f Dk(e-iX'~) g(x)dx = _(2'1T)-n/2 f e-ix·~Dkg(x)dx. - i~k,g(~) = (2'1T)-n/2 We write this fundamental identity as ./:: A ~ lSkg=Dkg· (2.17) * Using the finiteness of the domain of dependence of u on g (implied, e.g., by Holmgren's theorem), one can show that in the hyperbolic case the problem (2.14a, b, c) has a solution for gE C'(Rn), even without the assumption of compact support. t Here, of course, i = v=t . Observe that generally g is complex valued, even when the variables x,~,g are restricted to real values. In what follows the independent variables x,~ will be assumed to be real, unless the contrary is stated, but g,g, and the coefficients of the polynomial P will be allowed to be complex valued. 122 2 Higher-order Hyperbolic Equations with Constant Coefficients By repeated application we find more generally for g E multi-index a=(al, ... ,an ) with lal";; s that CO and any (i~)ag=t?g. (2.18) Thus differentiation for g is transformed into multiplication for g. Formula (2.18) permits us to show that g(~ decreases rapidly for when s is large. Let ~ = (~l' ... '~n)' where, say, ~--700 (2.19a) Then 1~I=y~~f ..;; 2sn s / 2 L ";;Vn lal';;s I~I (2.19b) (2.19c) I~al· Consequently (1 + I~IYI g (~)I..;; 2sn s / 2 ..;;2sn s/ 2 L lal<s l(i~tg (~)I L !IDag(x)ldx";; Ms <00, (2.20) lal.;;s where Ms depends on n,s, the size of the support of g, and the maxima of the absolute values of the derivatives of g of orders ..;; s. It follows in particular that forgECn+1(lRn) IgA(~)I~ Mn+l "" (I+IW n + 1 (2.21) and hence that the integral in (2.16) converges absolutely. Formula (2.16) is valid for s> n. Let now u(x,t) be a solution of (2.14a, b, c). To begin with we work with a single partial differential equation, so that u is a scalar. We write tentatively f u(x,t)=(2'1T)-n/2 eixo€fi (~,t)d~, (2.22) where u(x, t) is the Fourier transform of u with respect to x. Purely formally we obtain by differentiation f 0= p (D,'T)u(x, t) = (2'1T) -n/2 eixol;p (i~,'T)u (~,t)d~. 123 5 Hyperbolic equations in higher dimensions In addition for t = ° for k=O, ... ,m-2 f -{ :(X)=(2W)-"/2 e"'i(g)dE for k=m-l. These relations are satisfied formally, when solution of the ordinary differential equation u(~,t) for each ~ElRn is a (2.23a) P(i~,'T)U (~,t)=O with initial values for t = 0 for k=O, ... ,m-2 for k=m-l. (2.23b) This leads to the formal solution* of (2.14a, b, c) (2.24a) where Z as a function of t denotes the solution of the ordinary differential equation problem P (i~,'T)Z (~, t) = 0 (2.24b) with initial values for t = 0 for k=0, ... ,m-2 for k=m-l. (2.24c) There is no problem with the existence of Z. Moreover we can verify directly that the u given by (2.24a) is of class em in x, t for x ElRn, t ~ 0, and actually satisfies (2.14a, b, c), if g E q with s> n, and g and Z are such that all differentiations with respect to x or t of orders ..; m can be carried out under the integral sign in (2.24a). This is certainly the ~ase when the resulting integrals converge absolutely. For that it is sufficient that the expressions (1+I~Dn+II'Tk~az(~,t)g(~)1 forlal+k..;m (2.25) are bounded uniformly in ~, t for all ~ E IRn and for t restricted to any finite interval 0..; t"; T. Of course, the expressions (2.25) will be bounded in any bounded set in ~t-space. What matters is only the behavior for large I~I. Here, to a certain extent, g(~ can be controlled by assuming that s is large enough, as is *More precisely our arguments show that it there exists a solution u(x,t) of (2.14a, b, c) of compact support in x and sufficiently often differentiable, then u must be given by the expression (2.24a). 124 2 Higher-order Hyperbolic Equations with Constant Coefficients. shown by the estimate (2.20). It is just a question of the growth of Z (~, t) and its I-derivatives. If we can show that there exists a constant N, such that we find for the expressions (2.25), using (2.20), the upper bound (I +1~lr+l+m-sNMs. For the boundedness of the expressions (2.25) it is here sufficient to assume that s> n+ I+m. (2.27) Formula (2.24a) will then represent a solution of our standard Cauchy problem (2.l4a, b, c). The proper condition on the partial differential equation (2.l4a), i.e., on the polynomial P, under which an estimate of the form (2.26) holds, and hence the initial-value problem can be solved, is: Girding's hyperbolicity condition. Equation (2.l4a) is hyperbolic if there exists a real number c such that P (i~, iX) ~O for all ~ ERn and all complex X with ImX, - c. (2.28) Condition (2.28) is equivalent to the statement that all of the m roots X of P (i~,iX)=O (2.29) lie in one and the same half plane ImX> -c (2.30) of the complex number plane for all real vectors ~. * To establish the sufficiency of Garding's condition we represent the solution Z of (2.24b, c) by a Cauchy integral: Z (~, l iAr 1 e dX ) - 2'17" r P (i~, iX) , I - (2.31) where the closed path of integration r runs around each root X of (2.29) once in the counterclockwise direction. Indeed differentiation of Z as defined by (2.31) with respect to t results in mUltiplying the integrand by iX • Girding showed that his condition (2.28) is necessary as well as sufficient. An even stronger statement holds in the case where the polynomial P(D,T) is irreducible (i.e., not representable as product of lower degree polynomials): If the equation (2.14a) is not hyperbolic, the initial-value problem (2.14a, b, c) for gEq(Rn) never has a solution, unless g vanishes identically. 125 5 Hyperbolic equations in higher dimensions so that P{i~'T)Z=-21'TT 1 P{i~,{A) P r t") "N 1~,IA dA = _I r eiNdA=O 2'TT Jr by Cauchy's theorem, while for t=O by (2.10) TkZ=_I- ( ikAk dA. 2'TT r imAm+Pl{i~)im-lAm-l+ ... +Pm{i~) J Expanding r to infinity we see that this expression has the value 0 for k=0, ... ,m-2, and the value I for k= m-l. We first derive an upper bound for the roots A of (2.29). Using the expansion (2.10) we have P{itiA)={iA)m+PI{i~){iA)m-l+ ... +Pm{i~)=O (2.32) For each of the kth-degree polynomial Pk we have a trivial estimate IPk{i~)I' M{I + 1~ll for all ~ElIln with a suitable constant M. Then for a root A of (2.29) (2.33) m 1i\lm, M ~ (I + IwkIAlm-k. k=l Setting 0= IAI/(I + I~I), we have then om'M{1+0+02+ ... +om-I). This implies that either 0 < I or om, MmO m- 1 and hence 10 I< Mm. Thus for the roots A of (2.29) IAI 0= 1 + I~I < 1+ Mm. (2.34) Denote by Ak(~) for k= 1, ... ,m the m (not necessarily distinct) roots A of (2.29) taken in any order. Then m P{i~,iA)=im II (A-i\k{~»)' (2.35) k=l Take for each k = 1, ... , m the open disk of center Ak and radius 1 in the complex A-plane. Let U denote the union of these m (possibly overlapping) disks. Take for the path of integration r in (2.31) the boundary of U, which possibly consists of several closed curves and is composed of pieces of the boundaries of the individual unit disks. Then r runs once around each of the ~ and has total length ,2m'TT. Moreover each of the points A of r has distance # 1 from each of the Ak, so that by (2.35) IP{i~,iA)1 # 1 126 for AEr. 2 Higher-order Hyperbolic Equations with Constant Coefficients Since each point of f has distance 1 from some Ak we have from (2.34) and the Garding condition (2.30) ImA;> -c-I, IAI ~ 1 +(1 + Mm)(I +I~I) ~(2+Mm)(1 +I~I) on f. Thus fort;>O,AEf. leiAtI~e(l+c)t f It follows from (2.31) that 1 IrkZ(~,t)l= 2", ~ (iA)ke iAt P(i~,iA) dA m(2+ Mm)k(1 + IWke(l+C)T (2.35a) for 0 ~ t ~ T, ~ E IR n , 0 ~ k ~ m. This is an estimate of the type (2.26). It follows that for gE CO·+m+I(lRn) the initial-value problem has a solution of class em for t;> 0, provided the Garding condition (2.28) is satisfied. The integral (2.31) for Z is easily evaluated by the calculus of residues, in the case where all the roots Ak are distinct. One finds that then m . e tAkt"A Z(~,t)= '" £.J P C~ k=1 T 1 ,1 k r (2.36) As an example consider the n-dimensional wave equation corresponding to the operator n P(D,r)=O=r2-c 2 ~ Df. (2.37a) k=! Here (2.37b) has the real roots (2.37c) satisfying the Garding condition. Then by (2.35) Z (~, t) = sin(cl~lt) cl~1 (2.37d) Thus the standard problem for the wave equation has the solution (2.37e) for gE eO+ 3(lRn). If the polynomial P(D,r) is homogeneous of degree minD and r (as in equation (2.37a», we have for every solution (~,A) of (2.29) and every real s P(S~,SA)=O, Im(sA)=slmA. 127 5 Hyperbolic equations in higher dimensions Here sImA can be bounded from below for all s only, if ImA=O. Thus the Garding condition for homogeneous P is that all roots A of the equation P (i~,rA) = imp (~,A) =0 (2.38) are real for all real ~. In many cases hyperbolicity can be inferred from properties of the principal part of P alone. We arrange the terms in the polynomial according to their degree, writing P(D,r) =Pm(D,T)+Pm_I(D,T) + ... +PO(D,T), (2.39) where Pk(D,T) is a form of degree kinD and T. HerePm(D,T) is identical with the principal part of P(D,T) as defined in Chapter 3. We shall prove: For the Garding condition for P to be satisfied it is necessary that all roots A of (2.40) are real for all real ~ (i.e., that Pm satisfies the condition); a sufficient requirement which implies the Garding condition for P is that all roots A of (2.40) are real and distinct for all real ~+O. To prove this statement we apply the substitution ~= PT/, (2.41) A= pp., where p= I~I and T/ is a unit vector. Then P(i~,iA)=O goes over into the equation 1 Pm (T/,p.) + ip Pm-I(T/,P.) + ... 1 + {ip)m Po(T/,p.) =0 (2.42) for p., depending on the parameters p, T/. By (2.4) the coefficient of p. m in (2.42) has the value 1. The coefficients of the powers of p. not contributed by the principal part tend to 0 for P-'HXJ, since T/ is bounded. Using the fact that the roots of a polynomial with highest coefficient 1 depend continuously on the coefficients, we see that for p~oo the roots p. of (2.42) will tend * to the roots of (2.43) Let there exist for a certain T/ a root ILo of (2.43) with ImlLo+O. Assume 1m ILo = - y < 0 (otherwise replace T/ by - T/ and ILo by - /Lo). Then there exist roots p. of (2.42) for all sufficiently large p for which Imp. < - y /2 and hence roots A of (2.29) for which ImA < - py. This contradicts (2.30) for large p. Thus necessary for (2.30) is that the roots p. of (2.43) are real for all real'tJ with IT/I = 1, and then also for all real T/. Assume next that the roots p. are real and distinct for real T/+O, in particular for IT/I = 1. We now use the * More precisely in a given neighborhood of a root p. of (2.43) of multiplicity y there lie precisely y roots of (2.42) if p is sufficiently large. 128 2 Higher-order Hyperbolic Equations with Constant Coefficients fact that roots of a polynomial equation with highest coefficient one are differentiable (even analytic) functions of the coefficients in any region not containing multiple roots. They will be uniformly Lipschitz continuous in any compact subregion. For large p and 11J1 = 1 the coefficients of equation (2.42) for p. differ from those of equation (2.43) by terms of order 1/p. Hence the difference of the roots p. of (2.42) from appropriate roots of (2.43) is of order 1/p uniformly for 11J1 = 1. Since (2.43) has real roots, it follows that the imaginary parts of the roots p. of (2.42) are of order 1/p, and hence the imaginary parts of the roots A. of (2.29) are bounded uniformly for all sufficiently large p= I~I. By (2.34) A. and ImA. also are bounded for bounded I~I. Thus (2.30) follows. We call P strictly hyperbolic when its principal partpm(~'A.)=O has real distinct roots for ~~O hyperbolic. We see that strict hyperbolicity implies ~yperbolicity. Thus, for example, any equation of the form (2.44) uIt =c 2 b.+ku is hyperbolic. Formula (2.24) for the solution u(x, t) of the standard initial-value problem makes use of the values of g(~, which by (2.15) depend on the values of the given function g at all points. Actually by Holmgren's theorem the domain of dependence of u(x,t) on the values of g is known to be finite; equivalently initial data g of compact support lead to solutions u(x,t) of compact support in x. This is not obvious from the expression (2.24a), but can be deduced for strictly hyperbolic P from a version of the Pailey- Wiener theorem. This involves a shift in the integrations in (2.24a) to complex ~. From this we require estimates for the functions Z and g for complex arguments ~ + ir and real t >0, where ~ and r are real. Assume that the function g(x) belongs to CO (II~n) where s> n + m + 1, and that the support of g(x) lies in a balllxl < a. For the complex vector ~+ ir we define I~+ irl by I~ + ir 12 = n L I~k + irk 12 = 1~12 + Ir 12. (2.45) k=i Then as in (2.I9c) and by the same arguments (1+I~+irIY<2sns/2 L lal<s I(~+irtl (2.46) We conclude from (2.15), (2.18) in analogy to (2.20) that (1+I~+irIYlg(~+inl<2sns/2 Lf lal<s Ixl<a <2sns/2ealrl le-jx·(~+j.nDag(x)ldx L JIDag(x)ldx<ealrIMs' (2.47) lal<s 129 5 Hyperbolic equations in higher dimensions since for real x with Ixl < a Ie -ix.(€+iol = e x·r OS;;; elxllrlos;;; eo1rl. We proceed to estimate Z{~+·S t)- 27TI I, - 1 r e iN P(i{~+ in,iA) (2.48) dA using as path of integration r again the boundary of the union of the unit disks with centers at the roots Ak of P(i{~+in,iA)=O. (2.49) It follows, as in (2.35a) for k=O that IZ{~+is,t)los;;; me(l+c)t, (2.50a) where (2.50b) To estimate c we apply the substitution ~+ is = fY/1, A= PJL, (2.51) where p= I~+ i1J1 and 1J is a complex vector with 11J1 = 1. For a root A of (2.49) we obtain again equation (2.42) for JL. The coefficients in equation (2.42) differ from those in the equation Pm (1J,JL) =0 (2.52) by terms of order I/p. Since 1J=(~+in/p, and 1~/pl,ls/pl<1 the coefficients in the equation (2.52) differ from those in the equation Pm(~/P,JL)=O (2.53) by terms of order Isl/p. Since the roots JL of (2.53) are real, it follows for the roots JL of (2.42) that ImJL=O( I :Isl). Thus the roots A of (2.49) satisfy ImA=O(I+lsl)· (2.54) Since also as in (2.34). IImAlos;;; IAI =0(1 +I~+ is/)=O(I +p) is bounded for bounded p, we see that (2.54) is valid for all ~+ is. Thus there exists a constant M such that for the roots A= Ak of (2.49) 130 2 Higher-order Hyperbolic Equations with Constant Coefficients and hence, using (2.50a), (2.47) IZ(~+ in,t)1 ~ me(l+M+Mlfl t) leix-(~+inZ (~+ ir, t) g (~+ inl ~ mM e-x·f+t+Mt+(a+Mt)lfl s (1+1~IY (2.55) By Cauchy's theorem we can in (2.24a) shift the domain of integration from that of real to ~ + ir with fixed r without changing the value of the integral, due to the decay of the integrand for large I~I. Choose now r to be of the form ux/lxl, where 17>0. It follows from (2.24a), (2.55) that f lu(x,t)1 ~(2'1T)-n/2mMset+Mt-(J(lxl-a-Mt) (1 + I~I)-S d~. If here Ixl>a+Mt it follows for u~oo that u(x,t)=O. Hence u for each 1>0 has bounded support lying in the ball Ixl ~ a + Mt. The constant M here represents an upper bound for the speed of propagation of disturbances. So far we have dealt with the standard problem for a single scalar equation P(D,r)u=O. The case of a system of equations with constant coefficients requires only minor adjustments. If P is an N X N matrix satisfying (2.12) a formal solution of (2.14a, b, c) is again furnished by (2.24a), where now, however, Z (~, t) is an N X N matrix given by Z (~, t) = 2~ Irei>.t {p (i~, iA)-1 dA. (2.56) Here r has to be a path in the A-plane enclosing all singularities of the matrix P - I, that is, all of the mN roots Ak of the equation Q(i~,iA)=detP(i~,iA)=O. (2.57) Garding's hyperbolicity condition for systems states that there exists a constant c such that ImA> -c for all roots A of (2.57) for all real vectors ~. J. Hadamard introduced the important distinction between well-posed (also called correctly-set) problems and those that are ill posed (improperly posed, incorrectly set). The distinction applies specially to problems where a "solution" u is to be found from "data" g. Well-posed problems are those for which (a) u exists for "arbitrary" g. (b) u is determined "uniquely" by g. (c) u depends "continuously" on g. Here the words in quotation marks are somewhat vague and require that 131 5 Hyperbolic equations in higher dimensions the spaces of admitted functions u .and of functions g are specified. Typically well-posed problems are the Dirichlet problem for the Laplace equation and the initial-value problem for a hyperbolic equation with constant coefficients. * (see [27]). The initial-value problem for the scalar equation P(D,'T)u=O certainly is ill-posed when the principal part Pm of P does not satisfy Garding's condition, that is, when there exists a real vector 'I] and a nonreal scalar ILo such that We can assume here that ImlLo= - y<O, 1'1]1= 1. Consider for any s exponential solutions of the form (1 + I~I) -s-mei(xoHAt), where P(i~,iA)=O (2.58) and s is an arbitrary integer. Take here A=P/L· For sufficiently large P we can find a A for which I/L -1Lo1 < y /2. Then ~=p'l], IAI «11Lo1 + h )p, so that for t =0 and lal < s, 0 < k < in ImA< IDa.r"u1 = (I + p) -s-mIAlkl~al -hp, t «1 +p)-s-m(1 /Lol + h pk+la l «1+1 /Lo1+ ht, while u(O,t) = (I-I:p) -s-mleiAtI >(1 + p) -s-me ypt/2. Thus the initial data and their derivatives of orders < s are bounded l.miformly for all x, while u(Q,t)~oo for p~oo and any fixed t>O. Here u does not depend "continuously" on its initial data. PROBLEMS 1. For n=3 identify the solution of the standard initial-value problem for the wave equation given by (2.37e) with the solution u= tMg(x,ct) obtained from (1.14). [Hint: Compute Mg(x,ct) in terms of g from (2.l6).] *In the latter problem one can specify that u E em for x ERn, t;;. 0 and that g has uniformly _bounded derivatives of orders .;; s with s chosen sufficiently large. Then u depends continuously on g in the sense that the maximum of lui can be estimated in terms of the maxima of the IDQgl for lal.;; s. More generally the Cauchy problem with data on a space like surface is well posed. 132 2 Higher-order Hyperbolic Equations with Constant Coefficients 2. Solve the standard initial-value problem for the system of equations of elastic waves (2.59) (with positive constants p,A,JL) in the form (2.24a), computing the matrix explicitly from (2.56). [Answer: Z (~, t) is the matrix with elements Cl( ~ikl~12_~i~)Sin(C21~lt) + c2~~kSin(Cll~lt) Z(~,t) (2.60) where cr=(A+2JL)/p, ci=JL/p.] 3. Show that for n = 1, m = 1 and any N the system of equations Ut + Bux - Cu = 0 is strictly hyperbolic, when the matrix B has real and distinct eigenvalues. (Compare (5.12) of Chapter 2.) 4. Prove that, when Girding's condition is satisfied, the solution u of (2.l4a, b, c) can be written J u(x,t)=(1-~xY K(x-y,t)g(y)dy, (2.61a) where (2.61b) and s is any integer exceeding n/2. [Hint: Introducing h(x)=(l-~xJ'g(x), we can substitute for g in (2.24a) the expression (1 + 1~12)-Sh(~. Interchanging the integrations yields u(x,t)= JK(x-y)h(y)dy from which (2.61a) can be derived.] (c) Solution of a mixed problem by Fourier transformation In many cases mixed initial-boundary-value problems can be solved by Fourier transformation, when the domain of the solution is a half space. The method will be illustrated (following R. Hersh) by a problem for the wave equation for n = 3, which could also be solved by reflection. (Compare problem 3, p. 119.) We seek to find a u(x,t)=U(X 1,X2,x3,t) for which Du=O for X3>0, t>O u= ut =0 for X3 >0, t=O Mu= ut + a1ux , + a 2uX2 + a3uX3 = h(X 1,X2,t) for X3=0, t >0. (2. 62a) (2.62b) (2.62c) We assume here that the ak are constant, that a3 <0, and (to avoid inconsIstencies for t = X3 = 0) that there exists a positive e such that h(X 1,X2,t)=0 for t<e. (2.62d) 133 5 Hyperbolic equations in higher dimensions Let moreover h E CO (jR3) with a sufficiently large s. The building blocks are again exponential solutions u = ei(lu+€,x, +€2 X2+ €3 X3) (2.63a) of (2.62a), for which the relation (2.63b) A2-c2(M+M+~n=0 will have to hold. For these u we have Mu= i{A+ al~1 + a2~2 + a3~3)ei(lu+€,x,H2X2) for x3 =0. (2.63c) This leads to a formal solution of (2.62a,c) given by _ -3 / 2 f ei(lu+€,x, +~2X2+€3X3) ~ u{x,t)-{2w) .(A ~ ~ ~ ) h (~I'~2,A)d~ld~2dA. 1 +a 1 1+a2 2+ a 3 3 Here Ii is the Fourier transform of h: Ii (~1'~2,A)=(2w)-3/2 e-i(lu+~,x'+€2x2)h{Xl,x2,t)dxldx2dt f (2.64) (2.65) and ~3 in (2.64) is a function of (~1'~2,A) satisfying (2.63b). For convergence of the integral in (2.64) it is essential that the exponential in the integrand for each fixed t is bounded for x in the half space X3>0. This is the case, when ~1'~2 are real and Im~3 >o. (2.66) This condition does not fix the solution ~3 of (2.63b) uniquely for all real We also have to worry about possible vanishing of the denominator of the integrand. It is best to shift the integration with respect to A in (2.64) in the complex plane, letting A run through values with ImA = - 8 with a fixed real number 8 > o. Under these circumstances the solution ~3 of (2.63b) cannot be real, and there is a unique solution ~3' for which (2.66) holds. Moreover the denominator in (2.64) cannot vanish since ~1'~2,A. Im(A + al~l + a2~2 + a3~3) = - 8 + a 3Im~3 < - 8, (2.67) using (2.66) and the important assumption a3 < O. We obtain the estimate (2.68) for the absolute value of the integrand in the expression (2.64) for u. We now make use of assumption (2.62d), which implies that in the integral (2.65) giving Ii. We conclude, similarly as in (2.47), that for the complex A and real ~l' ~2 in question (2.69) with a suitable constant M. Thus for sufficiently regular h of compact 134 2 Higher-order Hyperbolic Equations with Constant Coefficients support formula (2.64) furnishes an actual solution of (2.62a,c). It remains to show that it satisfies (2.62b) as well. Now by (2.68), (2.69) MT f (1 +a+M+ IAI2fs d~ld~2dA. lu(x,t)1 <(2'1l-)-3/2 Letting 8-HX) 8(/-e) it follows that u(x,t)=O for X3>0, 0< t<e. This implies that (2.62b) holds. (d) The method of plane waves In what preceded the standard initial-value problem was solved by decomposing the initial function g(x) into exponentials exp(ix·~, according to Fourier's formula. For those the initial-value problem is easily solved; by superposition we then obtained the solution for general g. A disadvantage of this method is that the resulting solution u is expressed in terms of the Fourier transform g instead of directly in terms of g. For homogeneous partial differential equation with constant coefficients a different type of decomposition of g into plane waves can be preferable, since it does not involve the somewhat artificial introduction of exponentials. A function G with domain R n is called a plane wave function, if its level surfaces form a family of parallel planes, that is if G can be expressed in the form G= G(s), where the scalar argument s=x·~= ~~kXk (2.70) k is a linear combination of the independent variables. The exponential functions above are plane wave functions with G=e is • Assume that the differential operator P(D,T) is homogeneous of degree m, and thus agrees with its principal part Pm(D,T). Let P(O, 1)= 1 and the degree m of P be even. We notice that for any function G(s) of a scalar argument s we have in u(x,t)= G(x·~+At) (2.71) P (D,T)U = P (~,A)G(m)(x·~ +At). (2.72) a solution of In particular u will be a solution of P(D,T)U=O if ~,A (2.73a) satisfy the algebraic equation P(~,A)=O. (2.73b) We can find a linear combination of expressions (2.71) corresponding to the various roots A=Ak of (2.73b), satisfying the standard initial conditions 135 5 Hyperbolic equations in higher dimensions for t=O rku=O rm-1u= g for k=O, 1, ... m-2 (2.74a) for a plane wave function g=g{s)=g{x'~)' (2.74b) In the case where g(s) is an entire analytic function of s we easily verify that a solution is given by the Cauchy integral I u{x,t)= 2'1Ti J(G{x·~+i\t) P{~,i\) di\, r (2.75a) where the path of integration r in the complex I.-plane encloses all roots i\k of (2.73b). Here G is to be chosen so that G<m-I){s)=g{s). (2.75b) In the special case G (s) = eis we regain the formula u{x, t) = eix·I;Z (~, t) (2.75c) with Z given by (2.31). We now restrict ourselves to the case that P is strictly hyperbolic, that is, that all roots i\k of the homogeneous equation are real and distinct for ~ =1= O. In that case the calculus of residues permits us to evaluate the integral (2.75a) for ~=I=O: _ ~ G{x·~+i\kt) u{x,t)- .L.J . k=! P~{~,i\k) (2.76) Now formula (2.76) was derived under the assumption that G is analytic. By continuity arguments or direct verification it follows immediately that (2.76) represents a solution of (2.73a), (2.74a,b), when G is only of class cm(~) and satisfies (2.75b). Of special interest for us will be the case when g is of the form (2.77a) depending on parameter vectors (2.73a), (2.74a,b) is then given by _ U{x y,~. The corresponding solution u of _ ~ ({x-y)·~+i\kt)msgn({x_y)·~+i\kt) 'P (t I.) k=! m. ~ <;;, k y,t,~)-.L.J (2.77b) where we have used (2.76)* G{s)= ·Strictly speaking here harmless. 136 G~cm(R). (s- y.~)msgn{s- y.~) , . m. But the jump discontinuity in G(m)(s) for (2.77c) s=y'~ is 2 Higher-order Hyperbolic Equations with Constant Coefficients We shall show that for odd n and for s sufficiently large the general g(x)E Cooo(Rn) can be decomposed into functions of the form (2.77a) with I~I = 1 by a formula of the type g(x)= f..IEI=ldS(J 4Y1(x-y)-~lq(y) (2.78a) with a suitable continuous function q(y) of compact support. It follows then that u(x,t)= f..IEI=ldS€J 4Y U(x-y,t,~)q(y) (2.78b) solves our standard initial-value problem (2.14a,b,c).* To arrive at (2.78a) we first decompose the function r=lx-yl into plane waves of type (2.77a). This is achieved by writing x- y = rq, where 1111 = 1. (2.79a) (2.79b) Then (2.79c) Here Cn is a positive constant independent of 11, since a simultaneous rotation of 1I,~ does not change the integral of lI'~ over the unit sphere, so that we can always bring about that 11 is the unit vector in the xn-direction. By (1.9) of Chapter 4, i::.xri = j(j + n - 2)ri-2. It follows for odd n that there is a constant dn such that d i::.(n-l)/2r = n x 2-n r = K(x,y) (2- n)wn (2.80) is a fundamental solution of the Laplace equation with pole y (see Chapter 4, (1.l5a». Equivalently !. k(x,y)=dnr=cn-1dn I~I= 1 l(x-Y)'~ldS (2.81) is a fundamental solutiont with pole x for the operator ~n+l)/2: g(x)= f k(x,y)i::.~n+l)/2g(y)4Y. (2.82) Substituting for k its expression (2.81) we are led to a decomposition *Tbe U given by (2.77b) has continuous derivatives of order .;;; m with respect to its arguments, except for jumps in the mth derivatives. We use here that the P).. in the denominators are bounded away from 0 for I~I = 1, because P(~,A) has no multiple roots. tPormula (2.82) follows rigorously from (1.31) of Chapter 4 by integration by parts, provided gE q (IRn) with s;;. n+ 1. 137 5 Hyperbolic equations in higher dimensions (2.78a) for g with (2.83) With this q, formula (2.78b) solves the standard initial-value problem. PROBLEMS 1. Give the value for n = 3 of the constants [Answer: c3=2'17, d3= -1/8'17.] Cn> d" ~ formulas (2. 79c), (2.80). 2. Show that (2.78b) can be rewritten in the form u(X,t)=Cn-Id,,!~g(y)dy r J1cl =! ~U(x-y,t,~)dSc' (2.84) where m) . (n+l k=mm -2-'2 ' j=n+l_ k 2 (2.85) 3. For the wave equation (1.1) in n=3 dimensions identify the solution obtained from (2.84) with that given by formula (1.14). [Hint: Show that here i(x-yHi<ct for i(x-yHi>ct for flyU=l/c flyU=O i1€1=1 - - flyU(x y,t,~)dS~- {4'17t1i 4 1 x- yi '17 c for ix-yi >ct for ix-yi <ct. (2.86) Apply Green's formula.] 4. Show that for n = 3 dimensions formula (2.82) for g E CJ(JR3) takes the form g(x) = - ~flx 16'17 r JI~I=! dSc!i(x-yHiflyg(y)dy. (2.87) Show that here where G(~,p) (the Radon transform of g) denotes the integral of the function g(y) over the plane Y'~=p in JR3. Formula (2.87) solves the Radon problem of determining a function from its integrals over planes (for the case when g has compact support). Show how to obtain a different solution formula for this problem from Fourier's formula (2.15), (2.16) by expressing the Fourier transform g in terms of the Radon transform G. 138 3. Symmetric Hyperbolic Systems (a) The basic energy inequality In this section we shall be concerned with a linear first order system of P.D.E.s for a column vector u=u(x,t)=u(xl, ... ,xn,t) with N components U 1•• •• , UN' Such a system can be written symbolically in the form n Lu=A{x,t}ru+ ~ Ak{x,t)Dku+B{x,t)u=w{x,t). (3.1a) k=1 Here A,A I, ... ,A n,B are given N x N square matrices, w a given N-vector, and 7',D 1, ... ,Dn again stand for the differential operators 7'= a at' a DI = aX I ' ... , a Dn= axn ' As initial data we prescribe the values of u on the hyperplane t = 0 in xt-space. By a trivial substitution on u and w we can always bring about that the initial condition becomes (3.1b) u{x,O)=o. Following K. O. Friedrichs the system (3.1a) is called symmetric hyperbolic, if all of the matrices A,A1, ... ,A n (but not necessarily B) are symmetric, and moreover A is positive definite for all arguments (x, t) in question. We shall see that symmetric hyperbolic systems (for sufficiently regular A,A\ ... ,An,B,w) are indeed hyperbolic in the sense that the initial-value problem (3.la,b) can be solved. Many hyperbolic equations or systems can be reduced to symmetric hyperbolic form. Consider, for example, a single scalar hyperbolic secondorder equation n n Vtt = ~ aik {x, t)VX;Xk + ~ bi{x,t)vx,+c{x,t)v,+d{x,t)v, ~k=1 i=1 (3.2) where the aik form a positive definite symmetric matrix. We introduce here the vector u with the N = n + 2 components (3.3) ... , The n + 2 equations n n ~ aik7'Uk- ~ aik Dk Un + 1 =0 k=1 k=1 n 7'Un+l - fori=l, ... ,n, n ~ aikDkui - ~ biui-cun+l-dun+2=0, i,k=1 (3.4a) (3.4b) i=1 (3.4c) 139 5 Hyperbolic equations in higher dimensions are consequences of (3.2), (3.3). One easily verifies that they constitute a symmetric hyperbolic system. Similarly in Chapter 2 we were able for n = I to write general hyperbolic systems (3.la) in "canonical form," where A becomes the unit matrix and A J a diagonal matrix. This clearly implies a reduction of the system to symmetric hyperbolic form. Multiplying (3.la) with the transposed vector uT we find that* n T(uTAu)+ ~ Dk(uTA ku)+u TCu=2u Tw, (3.5a) k=l where n C=2B-TA - ~ DkA k. (3.5b) k=l Integrating (3.5a) over a region R in xt-space and applying the divergence theorem yields [:T( A: + ~> <:: )udS~ 1.{- uTeu + 2uTw)dx dt, (3.6) where dx J / dp, ... , dXn/ dp, dt / dp denote direction cosines of the exterior normal and dS the element of "area" of the boundary aR, while dx dt = dxJ ... dxndt is the element of volume of R. We define the slab R"h in xt-space for r..>O as the set R"h={(x,t)lxE~n,O<t<r..}. (3.7) Let for a certain T the function u(x, t) be a solution of (3.la,b) of class CJ(R T ), which is of compact support in x for each t in 0 < t < T. Applying (3.6) to R = R"h with 0 < r.. < T yields the energy identity E(r..)=f t=A uTAudx= fAdtf( -u TCu+2u Tw)d.x. )0 (3.8) We assume that the matrices A1A i, ... ,A n,B together with their derivatives of any desired order are continuous and bounded uniformly in R T • Moreover the matrix A shall be uniformly positive definite in the sense that there exists a /L > 0 such that (3.9) for all (x,t) in RT and all vectors v. Since C is bounded there will exist a constant K > 0 such that (3. lOa) ·We make use here of the symmetry of A,A I, .•. ,A n which implies T(uTAu) =( TU1)Au + uT( TA)u + uTA (TU) =2uTA (TU) + uTe TA)u and analogous identities for Dk(uTA "it). We tacitly assume thatA,A I, .•. ,A n are in C l , and B and w in Co. 140 3 Symmetric Hyperbolic Systems for (x,t)ERT and all v. Moreover, since A is symmetric and positive definite the inequality 2uTw < I-"UTu+ ~WTW < uTAu+ _1- wTAw I-" 1-"2 (3. lOb) holds for all vectors u, w. Thus by (3.8) E(A)«K+l)L h E(t)dt+I-"-2J. wTAwdxdt forO<A<T. o RA Writing this as (3.11) .!£e-(K+I)"" r""E(t)dt< e-(K+I)"" 1-"-2 r wTAwdxdt dA Jo JRr we conclude that io T e(K+I)T -1 J. E(A)dA< K 1 1-"-2 wTAwdxdt + Rr < JL- 2Te(K+I)T J. wTAwdxdt. (3.12a) Rr We define the inner product of two vectors u, v on RT by (u,v)= J. uTAvdxdt, and denote by II u II = y( u, u) Rr (3.12b) the corresponding norm. Setting (3.l2c) the estimate (3.12a) takes the form (u,u) < r2(w, w), (3.13) whenever u is a solution of (3.la,b) of compact support in x. Denote by ~s the space of functions uE CS(R T ), that vanish on t=O, and have compact support in x. Then by (3.13) the energy inequality (3.14) holds for all UE~I. The estimate (3.14) can be made the basis for an existence proof for the solution of the initial-value problem (3.1a,b). A first step in this direction is to establish the existence of a weak solution of that problem. For that purpose one introduces in analogy to ~ 1 the space (;1 of functions vEe 1(RT ) that are of compact support in x and vanish for t = T. For any u E ~ I, v E (;1 we derive by integration by parts Green's identity (see (4.5) of Chapter 3) (v,Lu) =(iv,u) (3.15) 141 5 Hyperbolic equations in higher dimensions where i, the adjoint of L, is defined by n iv= -T(Av)- ~ Dk(Akv)+BTv k=l = -Lv+(CT +B-BT)v (see (3.5a,b». A function u E C 1(RT) is a solution of (3.1a,b) if and only if (v,w)=(iv,u) (3.16) for all v E CI. For by Green's identity (not using (3.1 b), but using that v has compact support in x and vanishes for t = T) (iv,u)=(v,Lu) + J=ovTAudx. (3.17) Taking for v in (3.16) first an arbitrary function of compact support in RT and vanishing for t = 0, we see that u satisfies (3.1a). Subsequently we find from (3.16) that o=f vTAudx t=O for all v E Cl , which implies (3.1 b). This suggests replacing (3.1a,b) by the requirement (3.16) in some suitable function space. For that purpose we observe that C l is an inner product space (see p. 95), if we define as inner product of two vectors v and v' the expression (v, v') = (iv,iv'). (3.18a) Indeed this expression is linear and symmetric in v,v'. One only has to verify that the square of the corresponding norm 111·111 satisfies IIlvIW=(v,v)=(iv,iv»o (3.18b) for v*O. This is obvious, since - i is again a symmetric hyperbolic operator; replacing t by T - t the class Cl goes over into {; I. It follows in analogy to (3.14) that there exists a constant f such that -2 - - -2 (v,v)<r (Lv,Lv)=r (v,v), (3.19) which implies (3.18b). We complete Cl into a Hilbert space H, by taking Cauchy sequences of functions in Cl with respect to the norm Illvlll. Because of the inequality (3.19) we have for v in Cl and wE CO(RT ) that I(v, w)1 < I/vllllwi/ < fi/wl/lllvlll· Since by (3.19) Cauchy sequences with respect to the norm Illvlll also are Cauchy sequences with respect to the norm II vii, it follows that (v, w) defines a bounded linear functional on H. By the representation theorem (p. 96) we can then find an element U in H such that (v, w)=(v, U)=(iv,iU). 142 3 Symmetric Hyperbolic Systems Obviously then u=iu satisfies (3.16) for all vEH. This u, which belongs to the set of square integrable functions in R T , can be considered a weak solution of the initial-value problem (3.la,b). It remains, of course, to show that u can be identified with a strict solution in the ordinary sense, at least for sufficiently regular w. Here we shall not go into a proof of this fact, given in a classical paper by K. o. Friedrichs, * but shall instead give below an existence proof based on a completely different approach (also due to Friedrichs), namely the method of finite differences. In connection with proving regularity of solutions it is important to have "a priori" estimates for the values of a solution u and of its derivatives at each point (x, t) of RT" Such estimates can be obtained by first deriving estimates for the integrals of the squares of a sufficient number of derivatives. Those in tum can easily be obtained by using the differential equations satisfied by the derivatives. We find from (3.1a) and any i= I, ... ,n that Djw=DjLu= LDju + (DjA}ru + ~ (DjAk)Dku+(DjB)u. (3.20a) k Substituting still for 'TU its expression from (3.la) we see that Dju satisfies an equation of the form LDju= ~aikDku+biu+Diw+ejW (3.20b) k with certain square matrices aik,bi,ej, which by assumption are bounded in RT" There exists then an M such that IILDjul1 < M{; IIDkuli + lIull + IIWII) + IIDjwll· (3.20c) Assume that UE~2. Then DiUE~I, and we find from (3.14) that IIDiul1 <rM(; IIDkUII+llwll)+Mr21Iwll+flIDiWII. Summing over i yields ~ IIDiUl1 <rMn~ IIDkull+nMr(I+r)llwll+ ~ IIDiWII. k j (3.20d) i Now by (3.12c) the constant r can be made arbitrarily small by choosing T sufficiently small. Hence for sufficiently small T we have r Mn < 1/2, and conclude from (3.20d) that ~ IIDiUl1 <2nMr(I+r)lIwll+2nr~ IIDjWII· i i (3.21) A similar estimate can then be obtained for II'TUIl directly from (3.la). * Symmetric hyperbolic linear differential equations, Comm. Pure Appl. Math. 7, (1954), 551-590. 143 5 Hyperbolic equations in higher dimensions Forming next second space derivatives of (3.1a) and proceeding in this manner, we find that for sufficiently small T we can estimate all DClzl for 11001I<s in terms of the IID.Bwll for lfil<s (using, of course, the existence and uniform boundedness of the derivatives of the coefficients of L). Moreover by (3.11), (3.12b) we have for any UE~I and any A between 0 and T that [=>.uTAUdx=E(A) «K + 1)lluIl 2+ p. -21ILuIl2. Then for u E ~s by (3.9) [=>.(DClzl)T(DClzl)dx < p. [=>.(DClzl)TA (DClzl)dx -I < p. -I(K + 1)IIDClzlI1 2+ p. -311 LD Clzl11 2. This inequality permits us to estimate for any component uj of u and any 0: with 10:1 < s [=>.IDau/dx in terms of* the IIDflwll with 1131 < s. The transition from estimates for integrals of squares to pointwise estimates is furnished by one of the Sobolev inequalities. This inequality can easily be derived from Parseval's identity, known from the theory of Fourier integrals, that connects the square integrals of a function g with that of its Fourier transform g: (3.22) Let s=[l]+I, (3.23) where generally [v] for a real number v denotes the largest integer < v. Thus s is the smallest integer exceeding n12. By (2.16) and the Cauchy-Schwarz inequality g2(x)1 = (2.n 1 < Cn rn \f eix'~{l + I~I)-s{l + 1~lyg (~)d~\ 2 f (I + I~D2sl g(~)12d~, where cn=(2'IT)-n f {l + IW- 2s d~< 00. ·We use here that LD"u differs from D"w by a differential operator of order JaJ. 144 3 Symmetric Hyperbolic Systems By (2.20) (1 + 1~1)2'1 g (~)12..; 22sn' ( }: lal';;;' l(i~tg (~)1)2 ~, ";dn }: 1(i~tg(~W=dn }: ID ag1 2 , lal.;;;' lal';;;' with dn = 22sn' }: 1. lal.;;;s Using (3.22) with g replaced by Dag it follows that Ig2(x)l..; cndn L lal';;;s jIDag (Y)1 2dy. (3.24) Applied to the function g= u(x,t) for a fixed t between 0 and T, inequality (3.24) permits us to estimate lu(x,t)1 in terms of the IID.Bwll with 1.81..; s, with s given by (3.23). PROBLEMS 1. (a) Write the system (3.4a,b,c) in matrix notation and show that it is symmetric hyperbolic. (b) Do the same for Maxwell's equations (Chapter 1, (2.6a). 2. Show that a symmetric hyperbolic system (3.1a) with constant A,A 1, ... ,A nand B =0 satisfies the Girding hyperbolicity condition. 3. (Local uniqueness for the initial-value problem (3.1a,b).) Let bounded set in IRn, described by a function </>(x) for which </>(X»O for xEw, w be an open </>(x)=O on ilw. (3.25a) for A> 0 let R>. denote the "lens-shaped" region in xt-space given by (3.25b) xEw, and S>. denote the hypersurface xEw, t=A</>(X), (3.25c) so that R>. is bounded by S>. and SQ, Set (3.25d) (a) Show that for a solution of (3.1a,b) E(A)= r JR).. (-u T Cu+2uT w)dxdt. (3.25e) 145 5 Hyperbolic equations in higher dimensions (b) Call S" spacelike if the quadratic form in v Q" (v)= VT(A (x,/) - p. '± A k(X,/)q,Xk (X»)V (3.25f) k=l is positive definite for all (x, I) E S,.. (This is certainly the case for sufficiently small p..) Assume that the S" are spacelike for 0 < p. < A. There exists then a K such that (3.25g) for all v and all (x,/)ERA' taking p.=I/q,(x). Show that for a solution of (3.la,b) with w=O (3.25h) (c) Show that a solution of (3.la,b) is uniquely determined in RA by the values of w in RA, if the S" are spacelike for 0 < p. < A. Compare this result with Holmgren's theorem, p. 66. 4. Write the wave equation Ou=O as a symmetric hyperbolic system. Show that the definition of a spacelike surface using the form (3.25f) agrees with the one given by (1.54). 5. (a) Prove Sobolev's inequality (3.24) for n = 1 with cndn replaced by 2 from the identity (3.26a) (b) Prove by induction over the dimension n that for X=(XI'''''Xn ) g2(x)<2n L f(D g(y»2dy. a (3.26b) lal«n (b) Existence of solutions by the method of finite differences* We follow here the ideas and notations used on a trivial example in Chapter 1, p. 4. We cover (n+ I)-dimensional xt-space by a lattice. We take three positive quantities h, k, T, fixed for the moment, and consider the set ~ of points (x, t) for which x = (x], ... ,xn) = (a]h, ... ,anh), t = mk, 0 < t < T. (3.27) Here a], ... , a" , m shall be integers. It is convenient to combine the aj into a multi-index Ii = (a l , ... , an), where "-,, shall indicate that the components aj of Ii range ovt'lr all integers, in contrast to the common multi-indices a whose components shall continue to be nonnegative. Then ~ consists of the points x=lih, * ([18], [25D 146 t=mk withO<m< T/k. (3.28) 3 Symmetric Hyperbolic Systems We define operators Eo,~ corresponding to shifts to neighboring points: ~U(XI,.",Xn,t)= U(XI' ... ,xj + h, ... ,xn,t) forj= 1, ... ,n, Eou(x l , ••• ,xn,t) = u(x l , ••• ,xn,t+ k). (3.29a) (3.29b) Obviously ~ has the inverse ~ - I, where (3.29c) More generally combining (E1, ... ,En) into a symbolic vector E, we can write E"u(x, t) = u(x + iih, t) = U(XI + a1h, ... 'Xn + a"h,t). (3.29d) We next define divided difference operators 80, ~ by ~= E.-l T forj= 1, ... ,n Eo-1 80 = - k - (3.30a) so that, for example, 80 u(x,t) = U(X,t+ k) - u(x,t) k . (3.30b) For functions with continuous second derivatives these difference quotients approximate the corresponding derivatives, and we have by Taylor's formula ~U(X,t) = Dju(x,t) +O(h), 80 u(x,t) = Tu(x,t)+O(k). (3.31) It would appear natural to replace the differential equation (3.la) for the vector U by the difference equation n A80 v+ ~ A j8j v+Bv=w. (3.32) j=1 However in order to ensure stability, we have to select a more complicated difference scheme. We replace the space derivatives Dju by central difference quotients (2h)-I(~ - ~ -I)V, and, following Friedrichs, use instead of (3.32) the system of difference equations l( In ) In. AV="kA Eo- 2n ~ (~+~-I) V+ 2h ~ AJ(~_~-I)V+Bv=w. J=I J=1 (3.33a) Here it is understood that the argument of all functions is the same point (x, t), only shifted as indicated explicitly. The operator A is defined by 147 5 Hyperbolic equations in higher dimensions ° (3.33a). Equation (3.33a) is to hold for those (x,t) for which (x,t) and (x, t + k) belong to ~, restricting t to the interval ~ t ~ T - k. Since the matrix A(x,t) is nondegenerate, we can solve (3.33a) for Eov=v(x,t+k) in terms of w(x,t) and the v(y,t) with ~ IYi- Xii ~ h. i Thus formula (3.33a) constitutes a recursion formula that permits us to find v at the time t+ k if v and ware known at the time t. If we add the initial condition v(x,O)=o, (3.33b) then there exists trivally for given w a unique solution v(x,t) of (3.33a,b) in Obviously the value of v at any point (x, t) is determined already by the values of w(y,s) at a finite number of points (y,s), namely those for which ~. (3.34) The domain of dependence of vex, t) on w here has the shape of a pyramid with vertex (x,t- k). If, as we shall assume, w(y,s) has compact support in y for each s, then vex, t) has compact support in x. We are relieved of the burden of proving existence for v. Instead we shall have to show that v for h,k~O can be used to approximate a function u(x,t) defined in R T , which is a solution of (3.la,b). For that we shall need the "discrete" analogues of the energy inequality (3.14), of similar inequalities for higher derivatives, and of Sobolev's inequality. We shall make use of the same symmetry and regularity assumptions on the matrices A,A', ... ,An,B as before on page 140. We write (3.33a) as n AEov= ~ (aiEi+biE.i-I)v-kBv+kw, (3.35a) j=l where the matrices ai,IY' are defined by . 1 k· aJ=-A--AJ 2n 2h' (3.35b) The matrices aj, hi are symmetric. Since A is positive definite, the same holds for ai, hi provided the ratio k / h is sufficiently small. More precisely, using the fact that the Ai are bounded and A is uniformly positive definite there exists a positive A (held fixed in what follows) so small that the matrices ai, hi are positive definite for all (x, t) in R T , when the space and time steps are connected by k=Ah. (3.36) Now for a positive definite symmetric matrix a and any vectors v, w the 148 3 Symmetric Hyperbolic Systems inequality 2vTaw<2YvTav YWTaw <vTav+wTaw (3.37) holds.* (Compare (3. lOb).) Multiplying (3.35a) by 2EovT from the left, and using (3.37) for a = aj, b j we get 2(EovlA(Eov) «EoV)TC~1 (a j +~) ) (Eov) n + ~ ((~v)Taj(~v)+(~-lv)T~(~-Iv)) j=1 (3.38) By (3.35b) n L (aj+~)=A. (3.39) j=1 Moreover (~v)Taj (~v)= ~(vTajv) - (~v)T(~aj - aj)(~v) = ~(vTajv) - h(~V)T( ~aj)(~v). Now by assumption the derivatives, and hence also the difference quotients, of the aj are bounded uniformly for (x,t)ERT" Using (3.9), we can (after applying E) find a constant K such that (~v)T(8jaj)(~v) < K(~v?(~A)(~v)=K~(VTAv). Thus t Similarly ( ~ - IV) T ~ ( ~ - IV) = ~ - I ( v Tbjv) + O( h~ - I ( VTAv) ) (Eovl A (Eov) = Eo(vTAv) +O(kEo(vTAv» 2k(Eov)T(Bv - w)=O(kEo(vTAv) + k(vTAv) + k(wTAw»). * For a=urut matrix, relation (3.37) is just the Cacuchy-Schwartz inequality + the elementary inequality 2xy " x 2 + y2 valid for real numbers x,y. The case of more general a goes over into the previous one by writing a=cTc with a suitable matrix c. This amounts to writing the positive definite quadratic form vTav as a sum of squares. tWe use the customary notation F=O(G) to indicate that there exists a constant K such that 1FI .;; KG for all quantities F, G in question. 149 5 Hyperbolic equations in higher dimensions We then find from (3.38) that n Eo(vTAv)= ~ (~(vTajv)+~-I(VTbiv» j-I +0 [{~l (Ej + Ej-I)(vTAv) + k(vTAv) + kEo (vTA v) + k(WTAW))]. (3.40) We sum this inequality for a fixed 1 = mk over all x of the form ah. In analogy to the E (A) of (3.8) we introduce the energy sum .,,(1) =hn~ vT(iih,I)A (iih,I)V(iih,I) = h n~ E" (vTAv), (3.41) where ii ranges over all vectors with integers as components. Define similarly (3.42) Since, by assumption, w(x, I) is of compact support in x, our sums only contain a finite number of nonvanishing terms. Obviously we arrive at the same sum in (3.41), if vTAv is replaced by ~(vTAv) or ~-l(VTAv), since such a shift does not affect* the set of points over which we sum vTAv. Thus we obtain from (3.41), (3.40) that n .,,(/+k)=h n ~ (vTajv+vTbiv) j=1 + 0 (h.,,( I) + k'f/(I) + k'f/(I+ k) + kr (I» < .,,(/) + K(h +-k).,,(I) + k'f/(I + k) + kr (I» (3.43) . with a certain constant K. If k=Ah is so small that Kk< t, we can solve (3.43) for .,,(t+ k), and obtain an inequality of the form .,,(I+k) < eC~(I)+kyr(l) with certain constants C,y. Since .,,(0)=0, it follows for I=mk < T that .,,(/) < kyU (t- k)+ eCkr (t-2k)+··· + e(m-l)kcr(O») m < kye CT ~ ,,-0 r(pk). (3.44) *This observation plays the same role as did the integration by parts in the derivation of (3.8)_ 150 3 Symmetric Hyperbolic Systems In analogy to (3.12b) we define the norm IIwll of the vector w(x,t) for the lattice ~ by IIwll 2=h nk ~ (w(X,t»)T A(x,t)w(x,t)=k (x,t)E~ ~ O<m< T/k r(mk). (3.45) Summing (3.44) over all m with 0 <;; m <;; T / k we obtain the energy estimate IIvll2 <;; yTeCTllwll2= yTe CT IIAvl1 2 (3.46) in analogy to (3.14), (3.12c). The next step consists of deriving similar energy estimates for the difference quotients of v. (Compare (3.20a, b, c, d).) These are obtained by applying the operator 8, for r= 1, ... ,n to (3.33a). We make use of the rule for differencing a product of two functions U, V 8,(UV)=(E,U)(8,V)+(8,U)V (3.47a) and of the identity i (Eo- 21n j~1 (~+ ~-I) )v= (80- 21/\ -I j~18Al- ~-I) )v, 21h (~- ~ -1)= !(1 + ~-1)8j' (3.47b) (3.47c) We then find for 8, v an equation of the form A8, v = w' where w' is a linear combination of 8, w, wand the 8s v, ~ - 18s v with s = 1, ... , n. Applying the estimate (3.46) to 8,v instead of v, and summing over r, we arrive at an inequality of the type (3.48) provided T is sufficiently small. Repeating this procedure we arrive at estimates for the norms of the higher difference quotients: ~ lal<s 118avll2 = 0 ( ~ 118~112), (3.49) lal<s where we have combined the operators 81, ... ,8n into a vector 8, and write (3.50) Using (3.49), (3.9), we find then for any t = mk between 0 and T and any a with lal <;; s that also h n ~ (8 av( t3h,t))T( 8av( t3 h ,/)) <;; !l-Ihn~ (8 aV)TA (8 av) = o (IIA8 avI1 2) = 0 ( ~ 11'1<s IJ8YwI12). (3.51) 151 5 Hyperbolic equations in higher dimensions From the i 2-estimates (3.51) we pass to pointwise estimates by developing a difference analogue to Sobolev's inequality (3.24). This we can derive without recourse to Fourier transforms. (Compare problem 5, p. 146.) We start with the case n = 1 of a function g(x) of a scalar argument x. For a nonnegative integer r we have the identity r-l g(x)=g(x+rh)- ~ (g(x+(P+ I)h)-g(x+ph)) 1'=0 r-l =g(x+rh)-h ~ 8g(x+ph), 1'=0 where, of course, 8g(x) stands for (g(x+h)- g(x»/h. Squaring we get the estimate r-l g2(x),2g2(x+rh)+2rh2 ~ (8g(x+ph))2 1'=0 by Cauchy-Schwartz. Summing over r=O, I, ... ,p-I yields 00 00 pg2(x),2 ~ r= -00 g2(x+rh)+p 2h2 ~ (8g(x + rh))2. r=-oo We choose here for p the integer determined by 1 I h'P<h+1. For h sufficiently small, say h < V2 - I, we have p 2h2< 2, and hence 00 ~(x),2h ~ (g(x+rh)f+(8g(x+rh)? r= -00 (3.52) For x that are multiples of h we can replace x by 0 on the right. Next for a function g(x 1,X2) we find by repeated application of (3.52) that 00 g2(X),X2),2h ~ [(g(r)h,x2))2+(8)g(rlh,x2))2] rl= -00 ,4h 2 00 ~ [(g(r)h,r2h)f+(8)gi+(82g)2+(8)82g)2]. '1"2=-00 Generally for any n and for x of the form yh g2(X) , 2nh n ~ ~ (8 ag(,Bh)t lal<n ii It follows from (3.51) that for a solution of (3.33a, b) in 18 av(x,tW= 0 ( ~ Ipl<lal+n provided T (for given a) is sufficiently small. 152 118PwI12), (3.53) ~ and any a (3.54) 3 Symmetric Hyperbolic Systems We shall need estimates of the type (3.54) which do not depend on the particular values h which we shall let tend to O. For that purpose the expression IIB.Bw1l defined by (3.45) as a sum over ~ involving difference quotients of W will have to be replaced by an integral over RT involving derivatives of w. Let w have components WI' ••• ' Wn- Since A is bounded we have IIB.BwII=hnk ~ (8.Bw(X,t»TA (X,t)(B.Bw(x,t» (x,t)E~ ~ =O(hnk"i: r=1 (8.Bwr(X,t»2). (3.55) (X,t)E~ For the scalar Wr we have by the mean value theorem min DjwrCy,t)";; ~wr(x,t)";; max Djwr(y,t). Iy-xl';;h It follows by induction for min Iy-xl.;; sh Iy-xl.;;h IfJl..;; s that D.Bwr(y,t)..;; 8.BwrCx,t)";; max D.Bwr(y,t), Iy-xl.;;sh that is, that Bfiwr(x,t) = DfiwrCy, t) for some y with Iy - xl..;; sh. Thus hnk ~ (8 fiwr(x,t»2 (x,t)E~ is essentially a Riemann sum for the integral 1 (D.Bwr(x,t»2 dxdt. RT More precisely, for wr of classes and of compact support in RT the sum will converge to the integral for h---70. Consequently by (3.54) max I8"V(X,tW =O( (x,t)E~ L IPI.;;lal+n 1,D.Bw(x,tWdxdt) (3.56) RT for all sufficiently small h. We get similar estimates for the mixed spacetime difference quotients B~Ba by solving (3.33a) for Bov, using (3.4Th, c). In what follows we shall assume that w(x,t) is of class C n + 2(RT) and of compact support in x. Then v and all its difference quotients of orders ..;; 2 are bounded on ~ uniformly independently of h. This implies that v and its difference quotients of orders ..;; I are uniformly Lipschitz on ~, with a Lipschitz constant that does not depend on h. The rest is simple. We now refine our lattice ~ indefinitely, choosing h=2- q, k=A2-q with q=I,2,3,4, ... , while i\ is held fixed. We denote by ~q the lattice determined by these h,k and by vq(x,t) the solution of 153 5 Hyperbolic equations in higher dimensions (3.33a, b) defined on ~q' The ~q form a monotone increasing sequence of denumerable sets in IRn+l. Their union 0 is again denumerable. The function v q is define~ on all sets ~q' for q' <;; q .. The same holds for the difference quotients 8t,8 av q (where the operator 8t,8 a is formed with respect to the lattice ~q)' These difference quotients are bounded uniformly on ~q' for q' <;; q when i + lal <;; 2, and are uniformly Lipschitz, when i + lal <;; 1. From the boundedness it follows that there exists a subsequence S of natural numbers q such that liri:t 8~8avq(x,t)=ui,a(x,t) (3.57) qES q-+oo exists for i+lal <;; 1 and all (x,t)Eo. Moreover the ui,a are again uniformly bounded and Lipschitz on o. Since the set 0 is dense in RT , we can immediately extend the ui,a to all of the RT as Lipschitz continuous functions with the same Lipschitz constant as had been found for the 8~8avq. If we can prove that for (x, t) E RT and i + lal = 1 (3.58) then the difference equation Avq=w will in the limit for q-+oo in S go over into the differential equation Lu = w for u = uO,o, and we have solved our initial-value problem (3.Ia, b). Indeed rewriting (3.33a) with the help of (3.47b) and observing that q= E- 12- q8.2v q 8.(1E-1)v J J J J ui,a(x,t)=8iD~O,O(x,t) 1 -2 1 )8.v q = 8.v q (1 + E.J J J 1 -2 12- q8.2v q EJ J and using the uniform boundedness of 8/v q immediately yields the transition from (3.33a) to (3.Ia). We prove (3.58) for i = 1, a =O. The argument is the same for i = 0, lal=1. Consider at first two fixed points (x,t) and (x,t+c) of o. There exists then a q' such that (x,t) and (x,t+c) belong to ~q for all q;;. q'. Prescribe an e > O. We can find a q" > q' such that lu(x,t) - v q(x,t)1 < e, lu(x,t+ c) - v q(x,t+ c)1 < e for all q> q" belonging to S. (Here u stands for uo,o.) Thus u(x,t) _ vq(x,t+c)-vq(x,t) 1< 2e Iu(x,t+ c)c c c for q> q", q E S. Here c is a multiple of k = A2 -q, say c = mk. Then I I vq(x,t+c)-vq(x,t) 11 m-l c -8ov q(x,t) = m ,,~o 8ov q(x,t+vk)-8 ov q(x,t) =I! ~l "~l ,,=0 ,.=0 <;;Mmk=Mc, 154 8Jv q (X,t+pk)1 I 3 Symmetric Hyperbolic Systems where M is an upper bound for the second difference quotients of v q • Hence 12e - - - - - - 6ovq(x,t) .s;;;-+Mc. I-U(X,t+C)-U(X,t) c c Letting first q tend to 00 in S and then e tend to 0 we find that I - - - - - - u ' (x,t) .s;;;Mc I-u(x,t+c)-u(~,t) c i 0 whenever (x,/) and (x,t+c) belong to o. By continuity of u and ui,o this inequality holds then for any (x,t),(x,t+c) in R T • Letting here c tend to 0 yields the desired relation ru(X,t) = ui,O(x,t). This completes the existence proof for a solution u(x, I) of (3.1a, b) for where T is sufficiently small, under the assumption that wE C n + 2(R T ) and that w has compact support with respect to x.* o.s;;; t .s;;; T, PROBLEMS 1. Show that for the solution U of (3.1a, b) constructed here the domain of dependence of u(x,t) on w(x,t) is contained in the pyramid n I L IYr xjl.;;; X(t- s) 0.;;; s.;;; t. (3.59) j=i 2. Show that (3.1a, b) has a solution u(x,t) of class CS(RT) for sufficiently small T, if w is of class cs+n+i(RT ) and of compact support in x. 3. Let u be a solution of O.la, b) of class C n + 2(RT) and of compact support in x. Let v(x,t) be the solution of (3.33a, b) defined on the lattice r. Show that u(x,t)- v(x,t)= O(h) for (x,t) on r, provided T and k/ h are sufficiently small. (This implies that for w sufficiently regular we have vC~u for q~oo in any maimer, not just for q in a "suitable" subsequence S. Thus, in principle, we have a "construction" for u, a way to' find u numerically.) [Hint: Show that 8j U-Dj u=hfo'0dl} fo'drD/u(x+Orh) forj=l, ... ,n (3.60) with a similar formula for 80 u - Dou. This implies that Au - Av = h W, where W is of class C(RT ) and has compact support in x. Apply (3.56).] -The fact that the domain of dependence of u(x,t) on w is finite (see problem 3, p. 145 and problem I below) shows that the assumption of compact support for w is unessential. 155 6 Higher-order elliptic equations with constant coefficients* Here we can only indicate how some of the notions developed for the Laplace equation apply to more general elliptic equations. We shall restrict ourselves to a single linear homogeneous mth-order equation with constant real coefficients for a scalar function u(x)=u(x1, ... ,xn). We write the equation in the familiar form P(D)u=O, (0.1) P(D)= ~ AaDa lal=m (0.2) where is an mth-degree form in D =(D 1, ... ,Dn) with constant real coefficients Aa' Equation (0.1) is elliptic (see p. 58), if there are no real characteristic surfaces, that is, if (0.3). P(~)*O for all real ~*O. Weare only interested in the case when the dimension n is at least 2 and when the form P does not vanish identically. In that case the order m OJ the elliptic equation must be even. For taking any real vector r with p(n*O we can find a vector 1/ in ~n which is independent of r. Then P(q + is an mth-degree polynomial in t with leading coefficient p(n* o. Such a polynomial for odd m has at least one real root t, corresponding to a real ~ = 1/ + 0 with P(~ = O. Accordingly we shall set m = 2/1 with a positive integer /1. The expression pm/I~lm is homogeneous of degree 0, does not vanish on the sphere I~I = 1 and hence for all ~*O. Thus ellipticity implies the tn tr * *([1]. [2]. [12]. [15]. [20]. [21]) 156 I The Fundamental Solution for Odd n existence of a c> 0 such that (0.4) For convenience we shall write the partial differential equation (0.1) as Lu=( -I)"P(D )u=( -I)" ~ AaD"u=O. lal =2" (0.5) 1. The Fundamental Solution for Odd n A fundamental solution for L with pole y is a function F(x,y) satisfying LF=8y (1.1) in the distribution sense (see p. 69). For odd dimensions n it is easy to obtain such an F by the method of decomposition into plane waves described in Chapter 5, Section 5(d). We start with the observation that by (2.81) of Chapter 5 the function k(x,y)=dnr=dnix-yi (1.2) is a fundamental solution for the operator !l(n+ 1)/2: f (!l~n+1)/2V(X)k(x,y )dx = v(y) for every "test function" v E Cooo(\Rn). If then G(x,y) is a solution of LG(x,y)=r=ix-yi which has integrable derivatives of orders .;;;; n + m, we have in F(x,y) = dn!l~n+ 1)/2G(X,y) (1.3) (1.4) a solution of (1.1). For if v is a test function, and i is the operator adjoint to L, we have by Green's identity f f (Lv )Fdx= dn (Lv)!l~n+1)/2Gdx = dnf (!l~n+1)/2 Lv )Gdx = dnf (i!l~n+1)/2v )Gdx= dnf (!l~n+1)/2v )(LG)dx = f (!l~n+ 1)/2V )dnrdx = v(y). Ident~ty r(x,y,~ (2.79c) of Chapter 5 suggests the construction first of a solution of Lr=i(x-Y)·~i· (1.5) For then (1.6) 157 6 Higher-order elliptic equations with constant coefficients will be a solution of (1.3). Trivially _I(x - y )·~121'+ I f - (2JL+I)!P(~) satisfies (1.5), leading to --II l(x-y)·~121'+1 (2 + 1)!P(~) dSf.. If-I= 1 JL G(x,y)- cn Setting x - y (1.7) (1.8) = rq with 1711 = 1, we have 171·~121'+1 dS (1.9) (2 +1)!P(~) f.. I~I= 1 JL Clearly the integral in (1.9) is of class C 21'+ 1 in the vector 71. Actually it is C CXJ, even real analytic, in 71 for 1711 = 1. This can be seen by applying a suitable orthogonal transformation to the variable of integration ~. Choose a fixed unit vector ~. Let 71 be any unit vector linearly independent of ~. Then 71 and ~ span a 2-dimensional subspace 'IT of IRn. There exists a unique orthogonal transformation T (depending on 71 and of IRn which leaves all vectors orthogonal to 'IT fixed, rotates'lT in itself, and takes ~ into 71. Clearly C is determined by algebraic conditions, and must be analytic in 71 for real unit vectors 71~ ±~. (For an explicit expression for T see problem 1 below.) We replace ~ in (1.9) by T~, which changes neither the domain of integration nor the element of surface dSf.. Since G( x,y )- -121'+11 -Cn r n 71·T~= n·T~= ~.~, it follows that G( )- x,y - -121'+11 1~·~121'+1 dS r (2 + 1)!P(Tt) f.. If-I = 1 JL s Cn Since T is real analytic in 71 for unit vectors 71 ~ ± ~, the same follows for the integral. Since ~ was an arbitrary unit vector, we see that G is analytic in 71 for all real unit vectors 71=(x-y)/lx-yl. Thus the only singularities of G(x,y) for real arguments occur for r=O, that is, x=y. By (1.8) G(x,y) is homogeneous of degree 2JL+ I in x-yo A derivative of G of order k will be homogeneous of degree 2JL + 1 - k, hence integrable for k <. 2JL + n = m + n. In particular F(xy)=d c- 1a(n+I)/2 , n n x r J~ l(x-y)·~121'+1 (2JL+ I)!P(~) dS (1.10) f. If-I= 1 is homogeneous of degree 2JL - n = m - n, and hence is of the form for x-y=r71, (1.11) where cf>(71) depends analytically on the vector 71 for real 71 with 1711 near 1. We can draw up to JL of the Laplace operators in (1.10) under the integral F(x-y)=r m - n c/>(71) 158 1 The Fundamental Solution for Odd n sign, and obtain (1.12a) for n<m, and I(x-Y)'~I F(xy)=d c- 1Ll<n+l-m)/21 , n n P(~) x dS I; (l.12b) 1~1=1 for n>m. When the number n of dimensions is even, the analogue of formula (2.79c) of Chapter 5 for decomposition of functions into plane waves becomes more complicated. The result that a fundamental solution becomes singular like r m- n need not hold. Terms of the order rm-nlogr may occur. The simplest example is the fundamental solution (2'IT)-llogr for the Laplace equation in two dimensions. PROBLEMS t. Prove that the orthogonal transformation T described on p. 158 is given by T"=t._ a + b ,,+(1+2c)b-a 11 .. .. 1+ c ~ 1+ c ." (1.l3a) b=~·t (1.13b) where (Observe that T actually stays analytic in 11 for 1j = r, that is, c = 1.) 2. Let the Aa in (0.2) stand for square matrices with n rows and columns, so that (0.1) is an mth-order system for a vector u with n components. A fundamental solution matrix F satisfies LF= 8y I where I is the unit matrix. Prove that for odd n> m formula (1.l2b) represents a fundamental solution matrix if in the integrand we write P -1 instead of 1/ P. 3. Use problem 2 to find a fundamental solution for the equations of elastic equilibrium O=/L~ui+(A+/L) a:. (divu) (1.14) I (see (2.7) of Chapter 1). [Hint: Involved is the computation of the integrals (1.15) for 1111 = 1. Introduce This is a quadratic form in r. Show that for implies that Irl = I Q only depends on lI·r, which 159 6 Higher-order elliptic equations with constant coefficients for 1'111 = I, with constants a, b. Evaluate Q for '11 = unit vector in the x3-direction.]. 4. Find a fundamental solution of (1.l4) by finding a solution of the equations JL.1u;+(A+ JL) a:. (div)u)=F;(x) (1.l6) I for F; E ColX>, using Poisson's formula, (1.28) of Chapter 4, and the equations (A + 2JL).1(divu) = div F, .1r=2/r. [Answer: The fundamental solution matrix has the elements 5. Show that solutions of the elliptic equation (0.5) are real analytic in the interior of their domain of definition. [Hint: For odd n use the analyticity of the fundamental solution. For even n use Hadamard's method of descent adding a term ~:rl to P(g).] 2. The Dirichlet Problem The Dirichlet problem for the equation (0.5) of order m = 2p. consists in finding a solution u in the bounded region ~ for prescribed values of u and its first p. - I normal derivatives on a~, or equivalently for consistently prescribed values of u and its derivatives of orders ~ p.-l on a~. We can instead solve an equation of the form Lu=w(x) forxE~ (2.1) with w prescribed in ~, where u satisfies the homogeneous Dirichlet conditions D~=O for xEa~ and lal ~ p.-l. (2.2) We shall show how at least a weak solution of this problem can be obtained by following the Hilbert-space approach used in Chapter 4, Section 5. The method used here for homogeneous L with constant coefficients can be generalized to more general linear elliptic operators with variable coefficients. The key elements are the Girding inequality and the Lax-Milgram lemma. The passage from weak to strong solutions will not be attempted here. We denote by COOO(Q) the set of functions u E C OO(Q), whose support is contained in a compact subset of ~. Using as norm the expression lIuli = 1~ glal< p. IDaul2dx , (2.3) we can complete COO(Q) into a Hilbert space that will be called HP.(~). Completing the subspace COOO(Q) with respect to the same norm leads to a 160 2 The Dirichlet Problem Hilbert space HI)(Q) which we shall consider as the proper set of functions satisfying the Dirichlet condition (2.2) in the generalized sense. * We need to define an analogue B(u,v) to the bilinear form (5.13) of Chapter 4. For that purpose we decompose each multi-index a with lal=2,u in a trivial (nonunique) way into a=f3+y, where 1f31=IYI=,u. Writing (2.4) we have Lu=( -I)"P(D )u=( -1)1' L B/3,yD/3+yu=w = =" 1,81 Iyl (2.5) with certain B/3,y' Replacing, if necessary B/3,y by i(B,B,y + By,,B)' (again denoted by B,B,). we can bring about that B,B,y = By,,B' (2.5a) For any solution u E C 2"(Q) of (2.5) and any v E COOO(Q) we find by repeated integration by parts that k vwdx=B(v,u) (2.6) where B denotes the bilinear functional B(v,u)= IQI,8I=IYI=fL L B,BjD,Bv)(DYu)dx. (2.7) It is clear that for u E C 2"(Q) the partial differential equation (2.5) can be replaced by the requirement that (2.6) holds for all "test" functions v E COOO(Q). Here by Cauchy's inequality (2.8) IB(v,u)l..;; Kllvllilull with a suitable constant K. This inequality permits us to extend the domain of B(v,u) to all v,u in Ht;(Q). We just take Cauchy sequences of v,u in COOO(Q) with respect to the norm (2.3), and observe that the corresponding values of B converge by (2.8). The extended B is then again bilinear and satisfies (2.8). Similarly given wE C "(Q) the expression cJ>(v) = k vwdx (2.9) represents a linear functional in v satisfying 1cJ>(v)l..;; Ilvllllwll· (2.10) This functional also can be extended to HI)(Q) and is bounded because of (2.10). Our modified version of the Dirichlet problem is then to find a * HC(O) can also be obtained by completing the set CC(Q) of functions in CI'(Q) satisfying (2.2). 161 6 Higher-order elliptic equations with constant coefficients u E HC(fl.) such that cf>(v)=B(v,u) (2.11) for all v E Ht(fl.). The existence of u follows from the representation theorem on p. 96, if we can prove the existence of a positive constant k such that klluIl 2';;;B(u,u) (2.12) for all u E HC(fl.). For by (2.5a) the form B is symmetric: B(v,u)= B(u,v). (2.13) Moreover B(u,u»O for u*O by (2.12). Thus VB(u,u) = II lui II can be used as a norm on Ht(fl.). Because of (2.12), (2.8) (2.14) Thus the new norm is "equivalent" to the old one, in the sense that boundedness of functionals is the same in both norms. This applies in particular to the functional cf>(v), and the existence of u in (2.11) follows. It remains to establish (2.12). This is achieved most easily by Fourier transformation, making use of Parseval's identity «3.22) of Chapter 5) between a function g(x) and its transform t(g). More generally we have for two real-valued functions u, v in CoCXl(n) 4f u(x)v(x)dx= f[(U+V)2_(U-v)2]dx = f[lu(~)+ v(~)12_lu(~) - v(~)12] d~ =2 f (u;;3+ a13 )d~=4Re f u;;3d~. (2.15) It follows for u E CoCXl(n) from (2.7), «2.18) of Chapter 5), (2.5), (0.4) that B(u,u)= ~ 1.81=IYI=JL =Re = ~ Bp,yf(DPu)(DYu)dx 1.81=IYI=JL Bp,Yf«(i~)Pu)((i~)Yu)d~ f IPI=lyl=JL ~ Bp,y~P+Ylu (~)12d~ =f ~ Aa~alu(~)12d~ lal=2JL = f P(~)lu(~Wd~:> c fl~12JLlu(~)12dt 162 2 The Dirichlet Problem Since '5'. 1Pr=1' 1(i~).8uI2 ~ ~ 1~121'IuI2= q~121'1u12 IfJl=1' with a certain constant C, we find that B(u,u)~ ~f ~ 1(i~).8umI2d~ IfJl=1' =~f ~ (D.8U(X»)2dx. C IfJl=1' (2.16) Assume that {2 is contained in the cube Ix;1 ~ a for i = I, ... , n. Applying repeatedly Poincare's inequality «S.19a) of Chapter 4) we have for 0 ~ p ~ p. ~ f (D YU)2dx ~ ~ (2a)21'-2v f (Di- VDYu )2dx IYI=v IYI=/f ~(2a)21'-2v ~ f (D.8U)2 dx IfJl=1' and thus by (2.3), (2.16) I' lIu11 2 = /f~0 lyt,l'f(Dyu )2 dx ~ f (2a)21'-2v 1'=0 ~ IfJl=1' f(D.8u )2dx ~-kl B(u,u), (2.17) where (2.18) This establishes the inequality (2.12) for u E COOO(Q). It holds then clearly also in the completed space HC({2), thus proving the existence of a weak solution u of the Dirichlet problem. We give some indications for the analogous existence proof for more general linear elliptic equations Lu = w of order 2p., with coefficients depending on x. It is tlien natural to write the differential equation in the form Lu= ~ IfJ I< I' 11'1< I' (_1)I.8IB D.8+yu .8, Y (2.19) and to introduce the bilinear form B(v,u)= f ~ (D.8B.8,y v )(DYu )dx. 1.81" I' (2.20) IYI< I' 163 6 Higher-order elliptic equations with constant coefficients A weak solution of the Dirichlet problem can then again be defined as a u E HC(Q) for which (2.11) holds for all v E Hl)(Q). A difficulty about applying the representation theorem arises from the fact that now B(v,u) cannot be expected to be symmetric in v and u; (symmetry for the special case considered earlier arises from the fact that there the differential operator L is formally selfadjoint). This difficulty disappears, if we apply the Lax-Milgram lemma which assures us that in a Hilbert space Hl) any bounded linear functional cf>(v) can be written as B(v,u) with the help of a suitable u in the same space, provided the given bilinear form B satisfies inequalities (2.8), (2.12) for some positive constants k,K. (For a proof see [14], [11].) A further obstacle arises now from the circumstance that (2.12) just does not hold in general. If it did, the Dirichlet problem for the equation b.u + u = 0 would always be solvable, which is not the case. (See Problem 1 below.) What can be proved under suitable regularity assumptions is a weakened form of (2.12): Garding's inequality. There exists a positive constant k such that kllul1 2 ,,;; B(u,u)+ ~ u 2 dx (2.21) holds for all u E Hl)(Q). The integral on the right-hand side generally cannot be omitted. As a consequence there is no existence for the solution of the Dirichlet problem without some further qualification. Instead one obtains with the help of Garding's inequality a statement in the form of an alternative: Either there exists a nontrivial solution of Lu = 0 with Dirichlet data 0, or there exists a solution u of Lu = w with Dirichlet data 0 for every sufficiently regular w. PROBLEMS 1. Let n = 3 and Q be the ball Ixl < 17. Show that solution u of vanishing boundary values can only exist, if ~u + u = w(x) with (2.22) (compare problem 2, p. 79). 2. Show that for odd n the weak solution u of (2.5) constructed, is a strict solution in the region Q. [Hint: Usr the fundamental solution, as on p. 99.] 3. Consider a homogeneous system of equations with constant real coefficients of the form Lu=( -1)I'P(D )u=( -1)1' L JaJ=21' AuDuu=w, (2.23) where u and w are vectors with N components and the Aa constant square 164 2 The Dirichlet Problem matrices. Let L be strongly elliptic in the sense that there exists a positive c such that (2.24) for all real n-vectors ~ and N-vectors 1/. Write L in the form (2.5) and define B(v,u)= f 1.81 ~Iyl = = JL (DPvlBp,y(DYu)dx. Show that the "strong" Giirding inequality (2.12) holds for u E COOO(O) with a suitable positive k. [Hint: Show that B(u,u)=Re f uTp(~)Ctd~ ]. 4. Show that the system (1.14) is strongly elliptic in the sense of problem 3. 5. Show that if u E CIL(O) and u E Bg(n) then u satisfies (2.2). [Hint: For uk E CO(n) the identities (2.25) hold for lal..;; JL and all vE COO(O). Approximating uE COO(O) by certain Uk E COOO(O), in the sense of the norm (2.3) the identities (2.25) are preserved in the limit.] 165 7 Parabolic equations 1. The Heat Equation * (a) The initial-value problem The equation of heat for a function u= u(xI, ... ,xn,t)= u(x,t) has the form u/=k!!:..u (1.1) with a positive constant conductivity coefficient k. For n = 3 the equation is satisfied by the temperature in a heat-conducting medium. For n = I it holds for the temperature distribution in a heat-conducting insulated wire. The same type of equation occurs in the description of diffusion processes. Applying a suitable linear substitution on x, t we transform (1.1) into u/ =!!:..u (1.2) which will be used in the discussion to follow. Equation (1.2) is parabolic. A characteristic hypersurface cp(x,t)= tl{I(x)=O has to satisfy the degenerate quadratic condition (see (2.24) of Chapter 3) n ~ l{I; =0. k=I (1.3) ' Thus the only characteristic surfaces are the planes t = const. Unlike the usual equations in mechanics (including the wave equation), equation (1.1) is not preserved when we replace t by - t. This indicates that the heat equation describes "irreversible" processes and makes a distinction between past and future (the "arrow of time"). More generally, (1.2) is preserved under linear substitutions x' = ax, t' = a 2t, the same ones that * ([30)) 166 1 The Heat Equation leave the expression Ix1 2/ t invariant. Thus it is not surprising that the combination Ix1 2/ t occurs frequently in connection with equation (1.2). Important information is obtained by considering the exponential solutions with constant A and ~ = (~I' ... , ~n). Substitution in (1.2) yields the rdation iA= _1~12, and hence u(X, t) = eix·~-IH't (1.4) For each fixed t;;' 0 equation (1.4) describes a plane wave function, constant on the planes x·~=const. with unit normal UI~I, and repeating itself when x is replaced by x+2'1TUI~12. Thus the waves in (1.4) have wave length 2'1T L=W (1.5) and amplitude (1.6) The solutions (1.4) decay exponentially with time, except in the trivial case u = 1= const. We have tacitly assumed in (1.4) that the vector ~ is real, so that u for fixed t> 0 is bounded uniformly for x E~n. If we only consider our solutions in the half space XI ;;. 0, it is natural to require boundedness just in that half space, which leads to the condition that ~2' ... , ~n should be real and Im~1 ;;. O. For example for a real positive A ~ = 0, (1.7a) is such a solution when ~I = V - ill. = (- 1 + i)Vf . (1.7b) The corresponding "physical" real solution would be (1.7c) For n = 3 we can interpret v as the temperature below ground in a flat earth represented by the half space XI >0. Here v has boundary values cos"At for XI =0, which oscillate periodically with frequency A and amplitude 1. The resulting temperature at depth XI still oscillates with frequency A but with a phase lag v' (1 /2lI.) X I and with an amplitude 167 7 Parabolic equations exp( - V(>../2) xl) that decays exponentially with depth. Thus at the depth Xl =Vf log2 (1.7d) the amplitude will have decreased to ·1/2 its surface value. This "halfdepth" is inversely proportional to VX or proportional to Vii, where P = 2'17 />.. is the time period of v. Thus yearly surface variations of temperature can be expected to penetrate V365 times = 19 times as deep as daily variations with the same amplitude. The "pure" initial-value problem for the heat equation consists in finding a solution u(x, I) of (1.8a) ut-au=o for xElR n, 1>0 forxElR n , 1=0, u=f(x) (1.8b) where we require uEC 2 for xElR n, t>O, and uEC o for xEIR;n, t~O. A formal solution is obtained immediately by Fourier transformation. Writing f(x) = (2'IT)-n/2 f eix°o/(~)d~, (1.9a) we would expect on the basis of (1.4) that u(x,/) = (2'IT)-n/2 satisfies (l.8a, b). Substituting f eixo~-I~I¥(~)d~ (1.9b) f j(~) = (2'IT)-:n/2 e-iy°o/(Y)dy from Fourier's formula (2.15) of Chapter 5 and interchanging the integrations leads to u(x,/)= f K(x,y,t)f(y)dy, (1.10a) where (1.10b) The integral for K is easily evaluated by completing the squares in the exponent; introducing a new variable of integration 11 by ~= we find that 168 i(x-y) 21 1 + Vi 1/, 1 The Heat Equation Using the well-known formula f e- 11112 = (f_: e-i' cis drj r = 7T n / 2, (1.10c) we arrive at K(x,y, t) = (47Tt) -n/2e -lx-YI 2/4t. (1.10d) We shall verify directly that the u from (1.1Oa, d) satisfies (1.8a, b), without trying to justify the' steps in the formal derivation. In this we follow the model of the proof of Poisson's formula (Chapter 4, (3.9». Theorem. Let f (x) be continuous and bounded for x ERn. Then u(x,t)= f K(x,y,t)f(y)dy = (47Tt) -n/2 f e-lx-yI2/4'l'(y) dy (1.11) belongs to Coo for x ERn, t > 0, and satisfies ut = du for t > O. Moreover u has the initial values f, in the sense that when we extend u by u(x,O)= f(x) to t=O, then u is continuous for xER n, t~O. The proof follows from basic properties of the kernel K: for xERn,yER n, t>O. (a) K(x,y,t)EC oo (b) (~t -dx )K(x,y,t)=O (c) K(x,y,t»O (d) fK(x,y,t)dy=1 (e) For any 8 >0 we have for t>O for t>O forxERn,t>O lim! K(x,y,t)dy=O t-->O ly-xl>6 (1.12a) (1.12b) (1.12c) (1.12d) (1.12e) t>O uniformly for x ERn. Here (a), (c) are trivial from (1.10d), and so is (b) from (1.10b). Also, by (1.10d) substituting y = x + (4t)I/21j ( K(x,y,t)dy = 7T- n/ 2 ( e- ll1 l'd1j. )ly-xl>6 )1111>6/\1'4 t (1.13) When 8=0 this implies (d) by (1.10c), and implies (e) for 8 >0. Clearly these properties of K show that the u defined by (1.11) belongs to Coo and satisfies Ut = du for t > O. To prove that the extended u is continuous, at t=O we have to show that u(x,t)~f(f) for x~g, t~O. For 169 7 Parabolic equations e>O we can find a 8 such that If(y)-f(OI<e for ly-~1<28. Let M= sup If(y)l. Then for Ix-~1<8 lu(x,t)- f(~)1 = If K(x,y,t)(J(y) - <I <I ly-xl<8 f(~»~1 K(x,y,t)lf(y)-fml~+ ly-EI<28 I IY-xl>8 K(x,y,t)lf(y)-fml~ K(x,y,t)lf(y)- f(~)I~ +2M ( K(x,y,t)~ J1y - xl >8 < ef K(x,y,t)~+2M I IY- xl>8 K(x,y,t)~<2e for t sufficiently small. By the same type of argument one proves more generally that if f(x) is measurable and satisfies an inequality (1.14) for all x with fixed constants a, M then formula (1.11) defines a solution u(x,t) of Ut =Au of class COO for x ERn and 0< t< 1/4a. Here u(x,t)~ f(O for x~~ and t~O at every point ~ of continuity of f. We point out some important features of the special solution (1.11), (not the only one), of the initial-value problem (1.8a, b). We observe that u(x,t) for t > 0 depends on the values of f at all points. Equivalently the values of fnear one ~ a moment later affect the value of u(x,t) at all x, though only imperceptibly at large distances. Thus effects here travel with infinite speed, indicating some limitation on the strict applicability of the heat equation to physical phenomena. We notice from (1.12c,d) that for boundedf u(x,t) « f K(x,y,t)~)( s~p f(z») = s~p fez), and more generally that u satisfies the "maximum principle" inf fez) z < u(x,t) < sup fez) z for x ER n, t >0. (1.15) Here for continuous bounded f the equals sign can hold only when f is constant. The function u in (1.11) belongs to C 00 for any t > 0, even if the initial values f of u are only continuous, or even have jump discontinuities. More is true. For bounded continuousfthe function u(x,t) can be continued as an analytic function to all complex x, t with Ret> O. We only have to replace Ix-yl2 in the exponen.t in formula (1.10d) for K by the algebraic expression (x-y)·(x-y). Then for complex x=~+i'IJ, t=a+i'f', with 170 1 The Heat Equation ~,1'/,y,(1,T real, K(x,y,t) is analytic in x,t for t7"O, and moreover for (1)0 !K(x,y, t)! = (471") -n/2( (12+ T2) -n/4 exp ( _ Re = (~- y + ~1'/). (~~y + i1'/) ) 4 (1+ IT (1 + :: f/4eITJI2/4<JK( ~+ ~1'/,y,(1+ :). (1.16) It follows the for bounded continuous f from (1.12d) that f !u(~+ i1'/,(1 + iT)! < !K(~+ i1'/,y,(1 + iT)! ~ sup !f(z)! = ( zERn 2 I+~ (12 )n/4 eITJI2/40 sup !f(z)! zERn (1.17) for (1 > O. More precisely for bounded continuous f the function u(x, t) and its first derivatives are represented by absolutely convergent integrals for complex x, t with Re t > O. The analyticity of u follows (see p. 53). Thus after an infinitesimal lapse of time a temperature distribution u (at least if represented by (1.11)) is perfectly smooth, though of course, by continuity, it will approximate the changes in theinitial data. This smoothness of the future has as its counterpart that the past is likely to be rougher, as we shall see more precisely below. Values u(x,O)= f(x) that are not analytic in x cannot have originated at all by conduction from a temperature distribution in the past. Formula (1.11) represents only one out of infinitely many solutions of the initial-value problem (I.Sa, b). The solution is not unique without further conditions on u, as is shown by examples of solutions u E coo(lRn+l) of ut =/1u, which vanish identically for t<O but not for t>O.* Following Tychonoff we construct such u for the case n = 1. They are obtained by formally solving the partial differential equation ut = uxx for prescribed Cauchy data on the t-axis: u=g(t), ux=O for x=O. (US) Writing u as a power series DO U = ~ l5j( t)xj j=O • Conditions on u that imply uniqueness for the initial-value problem can take the form of prescribing the behavior of u(x,t) for large Ix!. as shown below. We also mention a result of Widder (see [30]) that there is at most one solution u which is nonnegative for t > 0 and all x. The assumption u > 0 is reasonable when u is the absolute temperature. 171 7 Parabolic equations we find by substitution into powers of x that Ut = gl=O, go=g, Uxx and comparison of coefficients of g;=(j+2)(j+l)~+2' This leads to the formal solutions (1.19) They will be actual solutions if the power series can be shown to converge sufficiently well. Choose now for some real a> I the g( t) defined by g(t)= {exp[ -0 t-a] for t>O for t"; O. (1.20) Convergence of the corresponding series (1.19) depends on estimates for the gk(t). These follow from Cauchy's representation for derivatives of analytic functions g(k)(t)= k!. r exp[ -Z-a] dz. 2m Jr (z _ t)k+ 1 (1.21) Here for a real t > 0 we choose for our path of integration a circle Iz - tl = fJt with a fixed fJ between 0 and I, and define za for Rez >0 as the principal value of that function, which is real >0 for real z>O. For z on r z = t + fJte i'" = t{1 + fJe hf ) Re{ - Z-a) = - t-a Re{1 + fJehf)-a with a real ",. Obviously we can choose fJ so small that Re{1 + fJehf)-a>~ (1.22) for all real '" and hence Re{ - z-a)< - it-a, Ig(k)(t)1 < ~ exp [ _It-a]. (fJtl 2 (1.23) Since k!/(2k)! < 1/ k! we observe that for real t >0 and any complex x Thus, by comparison, the series (1.19) for 172 U converges for real t>O and 1 The Heat Equation complex x, and, of course, trivially also for t < O. Formula (1.24) shows that limr-.ou(x,t)=O, uniformly in x for bounded complex x. The series (1.19) as a power series in x is majorised (see p. 61) by the power series for U(x,t)= { :x P[ 1 t 1- a )] 1 (X2 t 0 - 2" for t>O for t ~O. Since U(x,t) is bounded uniformly for bounded complex x and all real t, the series (1.19) converges uniformly in x,t for bounded x and real t, and the same holds for the series obtained by term by term x-differentiations. In particular the series co g(k)(t) co L X2k - 2= L k=2 (2k-2)! k=O g(k+l)(t) (2k)! X2k converges uniformly. Since this series is also obtained by formal differentiation of u with respect to t we find that ut = uxx ' More generally the relation (8/8t)kU =(8/8xfkU holds, which implies that uEcoo(~n+l). We observe that u is an entire analytic function of x for any real t, but is not analytic in t, since u(O, t) vanishes for t ~ 0 but not for t > O. PROBLEMS 1. Use formula (Lll) for n=1 to prove Weierstrass's approximation theorem: A function f(x) continuous on a closed interval [a,b] can be approximated uniformly by polynomials. [Hint: Define f(x) = feb) for x> b, f(x) = f(a) for x < a. Then u(x,t)~f(x) for t~O uniformly for a.;;; x.;;; b, since u is continuous for t;;. O. Approximate K(x,y,t) by its truncated power series with respect to x-y.] 2. Letf(x) have uniformly bounded derivatives of orders .;;; s. Show that the u(x, t) given by (Lll) is of class C S for t;;. 0 and all x. [Hint: Show that f D~= KD"jdy.] 3. Let f(x) be continuous in ~n and satisfy (Ll4). Show that the u defined by (Lll) is analytic in x, t for all complex x and complex t = (J + iT with (1.25) 4. Let u.(s,t), ... ,u,,(s,t) be n solutions of Ut=Uss ' Prove that (1.26) satisfies Ut = au. 173 7 Parabolic equations 5. Show that for n= 1 the solution of (1.8a, b) withf(x)= 1 for x>O,f(x)=O for x <0 is given by (1.27a) where q,(s) is the "error function" q,(s) = _2_1seVii tl dt. (I.2Th) 0 6. Show that for f(x) continuous and of compact support we have limr-.oou(x, t) = o uniformly in x for the u given by (1.11). 7. For n= lletf(x) be bounded, continuous, and positive for all real x. (a) Show that for the u given by (1.11) lu(g+i'l/,t)l..;; e'12 / 4tu(g,t) (1.28) for real g, '1/, t with t > 0; [Hint: (1.16).] (b) Show that el/ 2 luX<x,t)I..;;-- sup u(x+y,t) V2i lyl.;;v2i (1.29) (x,y,t real, t>O). [Hint: Use Cauchy's expression for uAx,t) as an integral of u over the circle of radius V2i and center x in the complex plane.] (This gives a means to estimate the maximum possible age t of an observed heat distribution u in terms of its maximum and its gradient, assuming that it has been positive and bounded for a time t.) 8. Find all solutions u(x, t) of the one-dimensional heat equation form u= Ut = Uxx of the Jt fC~ ). [Hint: f(z) has to satisfy a linear ordinary second-order equation, of which one solution f(z) = e- z2 is known, from u=K(x,O,t). All others can then be found by quadratures.] (b) Maximum principle, uniqueness, and regularity Let w denote an open bounded set of ~ n. For a fixed T cylinder Q in Rn+ I with base wand height T: Q= {(x,t)lxEw, 0< t< > 0 we form T}. the (1.30a) The boundary aQ consists of two disjoint portions, a "lower" boundary a'Q, and an "upper" one a"Q (see Figure 7.1): a'Q= {(x,t)leither xE aw, O~ t ~ Tor xEw, t=O} a"Q= {(x,t)IXEw, t= T}. (l.30b) (1.30c) As in the second-order elliptic case the maximum of a solution of the heat equation in Q is taken on aQ; but a more subtle distinction between the forward and backwards t-directions makes itself felt: 174 1 The Heat Equation a"n T a'n a'n a'n o w x Figure 7.1 Theorem. Let u be continuous in ~ and ut' UX,Xk exist and be continuous in g and satisfy ut -du ..;; O. Then (1.31) maxu= maxu. n PROOF. a'~ Let at first Ut-du<O in g. Let g, for O<e< T denote the set g.={(x,t)IXEW, O<t< T-e}. Since UECO(~,) there exists a point (x,t)E~, with u(x,t)= max u. n. If here (x, t) Eg. the n~cessary relations ut =0, du";; 0 would contradict ut-du<O. If (x,t) Eiy'g, we would have Ut >0, du";;O leading to the same contradiction. Thus (x, t) E a'g" and maxu= maxu..;;maxu. n. (l'~. a'~ Since every point of Q with t < T belongs to some g. and u is continuous in g, (1.31) follows. Let next Ut -du ..;; 0 in g. Introduce vex, t) = u(x, t) - kt with a constant positive k. Then vt-dv=u(-du-k<O and maxu= max(v+kt) ..;;maxv+kT= maxv+kT..;; maxu+kT. n n For k~O we obtain (1.31). n a'~ a'~ D 175 7 Parabolic equations The maximum principle immediately yields a uniqueness theorem n Theorem. Let u be continuous in a!!:.d ut ' UXiXk e:;cist and be continuous in n. Then u is determined uniquely in n by the value of Ut - 6.u in n and of u on a/no For the proof it is sufficient to consider the case where Ut - 6.u = 0 in and u = 0 on a/no Applying (1.31) to u and - u we find that maxu= max ( -u)=O, ~ n (1.32) ~ and hence that u = 0 in n. We can extend the maximum principle and the uniqueness theorem to the case where n is the "slab" n= {(x,t)lx E IRn, 0< t< T}, (1.33) if we assume that u satisfies a certain growth condition at infinity. Theorem. Let u be continuous for x E IRn, 0 < t < T, and let ut , Ux,xk exist and be continuous for x E IR n, 0 < t < T, and satisfy ut -6.u < 0 for 0< t< T, xE IRn (1.34a) u(x,t)<MealxI2 (1.34b) u(x,O)= f(x) forO<t<T,xElRn for xE IRn. Then u(x,t) <supf(z) z forO<t<T,xElRn. (1.35) It is clear that this theorem implies that the solution of the initial-value problem ut -6.u=O for 0< t< T (1.36a) u(x,O)=f(x) (1.36b) is unique provided we restrict ourselves to solutions satisfying lu(x,t)1 < MealxI2 for 0< t < T. (U6c) This shows that for bounded continuous f formula (1.11) represents the only bounded solution u of (1.8a, b). Obviously the Tychonoff solution (1.19), (1.20) for which u(x,O)=O cannot satisfy an inequality of the type (1.36c). By (1.24) it does satisfy such an inequality with the constant a replaced by 1/0t. PROOF OF THE THEOREM. tion that It is sufficient to show (1.35) under the assump- 4aT<1 176 (1.37a) 1 The Heat Equation For we can always divide the interval 0, t , T into equal parts, each of length T< 1/4a, and conclude successively for k=O, 1, ... ,T/T that U(x,/), sup u(y, kT) ,supu(y,O) y y for kT, 1 ,(k + I)T. Assume then (1.37a). We can find an e >0 such that 4a(T+e)< 1. Given a fixed y we consider for constants p, > 0 the functions (1.37b) vl'(x, I) = u(x,/) - p,(4'IT(T+ e- 1»)-n/2 exp[ Ix - Yl2 /4(T+ e - I)] =u(x,/)-pK(ix,iy,T+e-/) (1.38) defined for 0,1, T. Since K(x,y,/) as defined by (l.lOd), with Ix-yl2 replaced by (x-y)·(x-y), satisfies Kt=!J.K for any complex x,y,t with 1:;60, we find that ata vI' - !J.vl' = U -!J.u , O. (1.39) 0< t< T} (1.40) t Consider the "circular" cylinder Q= {(x,/)lIx- yl <p, of radius p. Then by (1.31) v..... (y,t) ,max V ... (j'{l ... (1.41) Here on the plane part of a'Q, since pK > 0, VI'(x, 0) ,u(x,O), sup J(z). z On the curved part (1.42a) Ix - yl = p, 0,1, T of a'Q by (1.38), (1.34b), (1.37b) vI' (x,t) = Me alxl2 - p,(4'IT(T+ e - t»)-n/2 exp[p2 /4(T+ e- I)] , Me o (lyl+p)2 - p,( 4'IT ( T+ e») -n/2e P2 /4(T+e) , supJ(z) z for all sufficiently large p. Thus max v"... 'supJ(z). (j'{l It follows from (1.41), (1.38) that vl'(y,t) = u(y,/) - p,(4'IT( T+ e - I») -n/2, supJ(z) For p,~0 we obtain (1.35). o In order to derive regularity properties of a solution of the heat equation in a bounded region we make use of Green's identity, as was done for harmonic functions on p. 76. Let again Q denote the cylindrical region (1.30a), where w is a bounded open set in IRn with sufficiently regular 177 7 Parabolic equations n boundary. Let u, up UXiXk exist and be con.!.inuous in and satisfy Ut - flu = O. For an arbitrary function v(x, t) E C 2(n) we find by integration by parts that 0= kv(ut -flu)dx = - ( u(vt+flv)dx+ f vudx- f vudx Jrl xEw xEw t= T t=O - (Tdtf (v du -udv)dSx • Jo xEilw dn dn For a certain ~Ew and e>O we choose (1.43) v(x,t) = K(x,~, T+ e- t), (1.44) so that vt +tJ.v =0. Then for f xEw vudx= f t=T e~O xEw K(x,~,e)u(x, T)dx~u(~, T), since by the theorem of p. 169 f (1.44a) f w(~,e)= K(~,x,e)u(x, T)dx= K(x,~,e)u(x, T)dx is a solution of w.-flgw=O with initial values* w(~,O)=u(x,T). Since also K(x,~,T+e-t) is uniformly continuous in e,x,t for xEaw, 0< t< T and for xEw, t=O, we find from (1.43) that f K(x,~,T)u(x,O)dx T f ( du(x,t) dK(X'~'T-t») + i dt d -u(x,t) d dS e~O, u(x,T)= w o xEilw K(x,~,T-t) n x' n (1.45) 1) We use this formula to extend u (~, T) to complex ~-arguments ~ = + iK (with K real), keeping T real. The first integral in (1.45) trivially is an entire analytic function of f Moreover for 0 < t < T, x =1= 1), 1) K(x,~, T- t)= (4?T(T- t»-n/2 exp [ - (x-~)'(x-~)/4(T- t)] is analytic in ~ and (see (1.16» bounded in absolute value by (4?T(T- t»-n/2 exp [ IKI:(j~~)1)12l. * The fact that x is integrated only over the region w instead over all of Rn does not change the proof given on p. 169, as long as ~ is a fixed point of w. 178 I The Heat Equation Thus K(x,~,T-t) is bounded uniformly for complex ~='I'/+i~ as long as Ix -'111 2-I ~ 12 is bounded below by a positive constant. The same holds for dK/ dn. In the second integral we first extend the t-integration from 0 to T - e and then let e~O. Since sequences of analytic functions which converge uniformly in a complex region have analytic limits, it follows that u(~,t) is analytic in~, as long as IX-'I1f-I~12>0 for all xEaw. This is certainly the case for complex ~ near a real point of w. It follows that u(~, T) is real analytic for ~Ew. More precisely u(~, T) is analytic for those complex ~ for which IIm~1 is less than the distance of Re~ from aw. Hence a solution u(x,t) of ut-du=O is real analytic in x in any open set where Ut and the UX,Xk are continuous. Moreover u(x, t) will be an entire function of x if defined for all real x and for 1 restricted to an open interval. We easily conclude that solutions of ut-du=O in an open set QElRn+1 belong to C OO(Q). For if u has continuous x-derivatives of all orders, then utxk = dUXk is continuous, and hence equals uxkt . Thus v = UXk also is a solution of the heat equation with the same regularity properties as u. The same holds again for VXk = UXkXk and then also for du = u(' Thus Utt = d~ is continuous. Proceeding in this manner yields that all derivatives of u(x, I) are continuous. As observed earlier analyticity of u(x,/) with respect to 1 cannot be expected. This fits in with the idea that the future of a heat distribution does not depend exclusively on the past, but also on outside influences that cannot be predicted. PROBLEM Let U be a solution of the one-dimensional heat equation Ut = Uxx in an open subset n of the xt-plane. Show that at a point of n there exist constants A,M such that I~;~ l";AM k (2k)! for all nonnegative integers k. [Hint: Use that U (1.46) is analytic in x.] (c) A mixed problem For n = 1 let u(x, I) be a solution of Ut - uxx = 0 in a half strip O<x<L 0<1. (1.47) We seek the u satisfying the boundary conditions u(O, I) = u(L,/) = 0 for I> 0 (1.48a) u(x,O)=f(x) (1.48b) and initial condition forO<x<L. Here u might represent the temperature in an insulated rod with the ends held at a constant temperature. This problem could be solved by Fourier 179 7 Parabolic equations expansion with respect to x, as was done for the wave equation in Chapter 2. A solution in closed form is obtained by reflection. We continue f(x) to all x so as to be an odd function of x and 2L - x: f(x)=-f(-x), f(x)=-f(2L-x). (1.49) We then solve the pure initial-value problem (1.Sa, b) with the extended* function f by formula (1.11). The resulting u(x, t) satisfies u,- uxx = 0 and the initial condition (1.4Sb). It also satisfies (1.4Sa) since u(x,t)+ u( - x,t) and u(x, t) + u(2L - x, t) are again bounded solutions of the heat equation with initial values 0, and hence vanish identically by the uniqueness theorem. Let cp(x) for x E IR be defined by for 0 < x < L for x < 0 or x > L. Then the extended f satisfying (1.49) is given by f( x) </>(x)= { 0 00 f(x)= L: L: ~ n= (</>(2nL+x)-</>(2nL-x). (1.50) -00 The corresponding solution (1.11) is u(x,t)= = K(x,y,t)f(y)dy K(x,y,t) n=~oo (</>(2nL+y)-</>(2nL-y)dy. Substituting 2nL +y u(x,t)= f oo =~, </>m 00 = respectively 2nL - y 00 ~ n=-oo =~, we obtain (K(x,~-2nL,t)- K(x,2nL-~,t)d~ foL G (x,~,t)f(~)d~, (1.51) where by (UOd) 00 G(x,~,t)= ~ n=-oo (K(x,~-2nL,t)-K(x,2nL-~,t) = _1_ ~ (e-<x-~+2nL)2/4'_ e-<X+€-2nL)2/ 4t). V4'ITt n = - 00 G can be expressed in terms of the classical theta-function ~3(Z,'T)= 1. f ~ n=-oo exp[ -i'IT(z+n)2/'T]. (1.52) *The extended 1 generally will have harmless jump discontinuities at the points x=mL, unless 1 satisfies the consistency conditions 1(0) = 1(L) =O. ISO 2 The Initial-value Problem for Second-order Linear Parabolic Equations We find (1.53) PROBLEMS 1. Find the solution of the one-dimensional heat equation u, = Uxx with boundary conditions (1.48a,b) by expanding u into a Fourier sine series with respect to x. Show that interchanging integrations we are led to the representation u(x,/) = fo LG (x,~, t)f(~)d~ with Show that the identity between the expressions (1.53), (1.54) is equivalent to the functional equation satisfied by the {l3-function: _0. "3 (Zr'--;I) =Vi ~ /T e i'1TZ2/T_o."3 ( Z,T.) (1.55) ° 2. Find a solution u(x,/) of the one-dimensional heat equation u,-UXX=O in the quadrant x > 0, I> satisfying the conditions u(x,O) =0, u(O,t)=h(/). (1.56a) [Hint: Apply formula (1.43) to the quadrant using v=K(x,~,T+e-t)-K(x, -~,T+e-t). (1.56b) For e_O, using (1.44a) we arrive at u(~, T)= (T ~ Jo ~ (T- t)3/2 e-e/4(T-')h(/)dt.] (1.56c) 2. The Initial-value Problem for General Second-order Linear Parabolic Equations* (a) The method of finite differences and the maximum principle Restricting ourselves to one space variable x, we consider a linear equation of the form Lu= Ut - a(x, t)uxx - 2b(x, t)ux - c(x,t)u = d(x,t). (2.1) *([11], [18], [25D 181 7 Parabolic equations We deal with solutions defined in a closed slab (2.2) J2={{x,t)lxER, o~ t~ T} and satisfying the initial condition (2.3) u{x,O)=f{x). To simplify statements we make the assumption that the coefficients a,b,c belong to C OO(~) and that they and each of their partial derivatives are bounded uniformly in ~. (Actually only a small finite number of derivatives will be required in each theorem). Most important is the additional assumption (the "arrow of time"), that the coefficient a(x,t) is positive and bounded away from in~: 0< inf a{x,t). (2.4) ° (X,t)E~ All results derived here will be based on the method of finite differences. The model is the discussion of symmetric hyperbolic systems in Chapter 5, Section 3. However, the present situation is greatly simplified by the existence of a maximum principle, which allows us to work with the maximum norm rather than with L 2-norms. Given two positive constants h, k we again consider the lattice ~ consisting of the points (x,t) with x=nh, t=mk O~t~ T (2.4a) with integers n,m. We replace (2.1) by the difference equation Av= v{x,t+ k)- v{x,t) v{x+ h,t) -2v{x,t)+v{x- h,t) k -a{x,t) h2 -2b(x,t) v(x+ h,t) - v(x- h,t) 2h - c(x,t)v(x,t)=d{x,t) for a function v(x, t) defined in the lattice condition v{x,O)= f(x) ~, (2.5a) and satisfying the initial for x=nh. (2.5b) Solving for v(x, t + k) we write (2.5a) in the form v(x,t+ k)= (Ail + hAb)v(x+ h,t) +(1-2Ail+ h2AC)V{X,t) + (Ail - hAb )v(x - h,t) + h2Ad(x, t), (2.6) where we have set A=kjh2 (2.7) and a,b,c are taken at the point (x,t). Introduce the norm II gil = sup Ig(x)1 x (2.8) for a bounded function g (here defined for x = nh only). Introducing the 182 2 The Initial-value Problem for Second-order Linear Parabolic Equations shift operators E,l1 defined by Ev(x, t) = v(x + h, t), ."v(x,t) = v(x,t+ k) (2.9) a solution of (2.6) clearly satisfies I11VI" [IAa+ hAbI +i1-2Aa+ ~2ACI +IAa- hAbI ]llvll + klldll. (2.10) Assume now that A= k / h 2 is so small that the stability condition 2A sup a(x,t)<1 (2.11) (x,t)E::£ is satisfied. Then since (2.4) holds and b,c are bounded, IAa+"hAbI + 11-2Aa+h 2ACI +IAa-hAbI = I +h2Ac= I +kc for all sufficiently small h. Setting C=max(O, s~pc(x,t)), (2.12) II11Vll ,,(I + kC)lIvll + klldll, (2.13) we find from (2.10) that where IIvll and IIdll depend on t=mk. Introduce the norm IIldlll = sup IIdll = sup Id(x,t)l. (x,t) E::£ t (2.14) Then iterating the inequality II11Vll ,,(1 + kC)llvll + kllldlll, and using the initial condition (2.5b), we arrive for t = mk at the estimate IIvll ,,(I + kC)mllfll + "emkcllfll + b((1 + kC)m-1)lIl d lll .1 (e mkC -l)lIldlll C "eCtIIfII + teCtllldlll· This proves: Lemma I. If A= k / h 2 satisfies the stability condition (2.11) and if h is sufficiently small, then the solution v of (2.5a,b) satisfies the "maximum principle" ° (2.15) [This implies in the case d=O, c" that the supremum of Ivl in ~ is the same as the supremum on the initial line.] Let now u(x,t) be a solution of (2.1), (2.3), for which u,ut,ux,uxx are uniformly bounded and uniformly continuous for (x,t)E~. Choose a fixed A for which (2.11) holds. Consider the monotone increasing sequence of 183 7 Parabolic equations lattices l:" corresponding to the choices h-2-", k_'J\2-2" for 11-1,2, .... Denote by v" the solution of (2.5a,b) corresponding to l:". If U is the union of all l:" and (x,t) a point of U, then v"(x,t) is well defined for all sufficiently large 11. Under these assumptions we have Lemma D. For each (x,t)E U lim v"(x,t)-u(x,t). (2.16) " ..... 00 PROOF. By Taylor's -theorem and the uniform continuity assumptions u(x,t+k)-u(x,t) k -u,(x,t) (2.17a) u(x, +h,t)-u(x-h,t) k -uAx,t) u(x+ h,t)-2u(x,t)+ u(x- h,t) h tend to 0 for given e>O h~O, k~O 2 - (2.17b) uxx(x,t) (2. 17c) uniformly for (x,t)ESl. This shows that for a IAu-dl<e for all (x, t) E l:" provided 11 is sufficiently large. (Here the difference operator A is the one corresponding to the lattice l:".) Since v" satisfies (2.5a) it follows that IA(u-v")1 <e. Using that u-v"-O for t=O, and applying (2.15) to u-v", we find that lu(x,t) - v"(x,t)1 <;; eTe CT (2.18) for all (x, t) El:" provided 11 is sufficiently large. This proves Lemma II. 0 Since each v"(x,t) satisfies (2.15) for (x, t) El:" and we see from (2.16) that also lu(x,t)1 <;; e CT ( sup Iii + Tsup Idl) 11 sufficiently large, (2.19) n for all (x,t)E U. The same inequality holds then for all (x,t)ESl because of the assumed continuity of u. We notice that the stability condition (2.11) requires the "mesh ratio" k / h to tend to zero, as we refine the mesh and let h and k tend to O. This requirement is to be expected from the Courant-Friedrichs-Lewy test (p. 6), if we want the solution of the difference scheme to approximate that of the differential equation. Indeed bounded h / k would correspond to a uniformly bounded domain of dependence for v"(x,t) oni, and hence also for u(x,t), whereas the example of the heat equation shows that the IR 184 2 The Initial-value Problem for Second-order Linear Parabolic Equations domain of dependence of u(x,t) on the initial values is the whoie x-axis. That the stability test involves a numerical bound on ak I h 2 is plausible since this combination is dimensionless; [a(x,t) is of dimension x 2 1t by virtue of the differential equation (2.1)]. We can dispense with the uniform continuity assumptions in (2.19): Theorem. The inequality (2.19) holds for a solution u of (2.1), (2.3), if U, Ut ' UX ' Uxx are continuous and u, Ux are uniformly bounded in ~. PROOF. We introduce a "cutoff function" cf>(x) ECCO(IR) for which 0, q,' I for all x, while q,=0 for Ixl>2 and q,=1 for Ixl<l. Then for r>O the function u r (x, t) =q,(x I r)u(x, t) agrees with u for Ixl < r and vanishes for Ixl >2r. ur,u;,u;,u;x are uniformly continuous and uniformly bounded in ~. Moreover u r satisfies Lu r =q,d- 2ar- 1q,'ux - (ar- 2q," + 2br- 1q,')u= d*, lur(x,O)I'lu(x,O)I=lf(x)l· Thus by (2.19) applied to u r lur(x,t)I' e CT ( sup If I+ Tsup Id*I). IR Q (2.20) Since u, Ux are bounded uniformly we have lim sup Id*1 = sup Idl, r---"oo Q Q o and (2.19) follows for u from (2.20). The theorem trivially has the consequence that the solution of the initial-value problem (2.1), (2.3) is unique, if we restrict ourselves to solutions u for which u and Ux are bounded uniformly. (b) Existence of solutions of the initial-value problem Here we closely follow the pattern of the existence proof given in Chapter 5 for symmetric hyperbolic systems by the method of finite differences. We only need to sketch the arguments. We assume that the prescribed functions f(x) and d(x,t) together with their derivatives of orders ,4 are continuous and uniformly bounded for xEIR (respectively (x,t)E~). Without ambiguity we shall now use the notation IIfll= suplf(x)l, IR IIldlll= supld(x,t)1 Q (2.21) in the case of functions defined for all x (respectively all (x, t) E~). The suprema of these functions in a lattice do not exceed these values. Let again v denote a solution of (2.5a,b), where it is assumed that (2.11) 185 7 Parabolic equations holds and that h is sufficiently small. We then have the estimate (2.15) for vex, I) in ~. We can obtain analogous bounds for the difference quotients of v. Let w(x, I) be defined in ~ by I w= 8v= h(E-I)v= v(x+h,/)-v(x,/) h . (2.22) Using the product rule 8 (ab) =(Ea)8b+ (8a)b, (2.23) we find from (2.6) that w satisfies the equation w(x, 1+ k) = E (Aa + hAb)w(x + h, I) + E (1- 2Aa + h2AC)W(X, I) + E (Aa- hAb)w(x- h,t)+ 8(Aa+ hAb)v(x+ h,/) + 8(1-&+ h2AC)V(X,t) + 8 (Aa- hAb)v(x- h,/) + kM(x,/) = E (Aa+ hAb)w(x+ h,/) + E(I-2Aa+ h2AC+ hE- 1 8(Aa+ hAb»w(x,/) + E(Aa- hAb - hE -18 (Aa- hAb»w(x- h,/) +k(8c)v+M). Since 8a, 8b, 8c, are bounded uniformly by Illaxlll, IlIbxlll, lilexill respectively, we find for A satisfying (2.11) and h sufficiently small that Iw(x,l+ k)1 <(1 + kEc+2k8b)lI w ll + k(18cllvl + IMI) <(1 + kC + 2klllbxlll)lI w ll + k(lllexllllllvlll + Illdxlll)· Since w(x, 0) =1, it follows as before that 1I18vlli = IIlwlll < e(c+21I1 bxlll)T (111xll + T(lllexllllllvlll + Illdxlll)), (2.24) where for Illvlll we have the estimate (2.15) in terms of 11111 and Illdlli. Similar estimates clearly can be obtained for the higher difference quotients 8 2v, 8 3v, 8 4v, and then also by (2.5a) for I ( ) 'Tv=7(1J- Iv = v(x,l+k)-v(x,t) k ' (2.25') and for 8'Tv, 8 2'Tv, and 'T2V. All these are bounded uniformly. As before we define the increasing sequence ~P of lattices and the corresponding solutions v P defined in ~p. Then v P, 8v P, 8 2v p , 8 3v p , 'TV P, 8'T2V Pare defined and bounded uniformly in ~P' and hence also in ~I' for IL < P. For a suitable subsequence of the integers p lim vP(x,t)=u(x,/), 11--+00 lim 8 2v p (x,t)=U"(x,/), JI--+ 00 186 lim 8v P(X,/)=U'(x,/), 11--+00 lim'TVP(x,t)=u(x,/) P-HX) 2 The Initial-value Problem for Second-order Linear Parabolic Equations exist for all (x, t) in the union U of the ~p. Let (x, t), (y, t) be two points of U, and hence of ~P' for all sufficiently large P. Then for O<y-x=hn= n2- P I - - - - - -8v (x,t) I-vP(y,t)-vP(x,t) y-x P =lvP(x+nh,t)-vP(X,t) _ vP(x+h,t)-vP(x,t) nh h =I( I E:;l - E;1 )vpl =! (E~ll (En-2+2En-3+3En-4+ ... +n-l)V P ! = 1~(En-2+2En-3+ .. . + n-l)~2vpl' , en ~ l)h 111~2VPIII ly~xlll182vPIII ,Kly-xl with a constant K independent of v. In the limit for subsequence we obtain the inequality I - - - - - u ' ( x , t ) 'Ciy-xl I-U(y,t)-U(X,t) y-x V-H~) in the (2.26) for all (x,t), (y,t) in U. Since v P, 8v P, 8 2v p, 'TV are uniformly Lipschitz in ~P' the limits u,u',u",it are uniformly Lipschitz in U, and hence can be extended as continuous functions to all of n. By continuity then (2.26) holds for all (x,t), (y,t) in n. For y-7X we find that uxCx,t) exists and that P uxCx,t) = u'(x, t). Similarly one verifies that Uxx = u", Ut = it, and that the differential equation (2.1) is satisfied. This proves the theorem: Theorem. If f, d and their derivatives of orders ,4 are continuous and bounded uniformly, the initial-value problem (2.1), (2.3) has a solution u(x,t), for which u,ut,ux,uxx are uniformly bounded and uniformly continuous in n. In conclusion we observe that there are many results we derived for the heat equation which one would expect to be valid for more general equations of the form (2.1). For example the solution of (2.1), (2.3) should be unique under the sole assumption that u, Up Ux' Uxx are continuous and that u is bounded uniformly. We would also expect the solution of the 187 7 Parabolic equations homogeneous equation Lu = 0 to exist and to be in Coo for 0 < t '" T, if f is only assumed to be continuous and bounded (always requiring a,h,c to be in Coo and bounded, and a to be positive and bounded away from zero). However, such questions are beyond the scope of this volume. PROBLEMS 1. Let u(x, f) be a solution of class C 2 of U1 = a(x,t)uxx + 2b(x,t)ux + c(x, f)u in the rectangle n= {(x,t)IO< x < L, 0 < t < T}. Let a'n denote the "lower boundary" of n consisting of the three segments x=O, 0< t< T O<x<L, t=O x=L, 0< t< T. (a) Prove that in case c<O in n lu(x,t)1 < sup lui for (x,t) En. a'Sl [Hint: Show maxgu cannot be assumed on (b) Show that more generally n- a'n unless maxgU < 0.] (2.27) where C=max(O, maxiel). Sl [Hint: Substitute u= e'Ylv, where y> C, and apply part (a) to v.] 2. Let u(x,f) denote the solution (1.11) of Lu=Ut- uxx=O for 0< t < T (2.28a) u(x,O) = f(x), (2.28b) where f is continuous. Let ~ denote the lattice of points (x,t) with x,t of the form x = nh, t = mk and v the solution of v(x,t+ k)-v(x,t) v(x+ h,t)-2v(x,t)+ v(x- h,t) =0 (2.29) k h2 with v(x,O)= f(x). Av= (a) Show that for A=k/h 2 =1/2 v(nh,mk)=2-m f j=O (~)f«n-m+2j)h) J and hence sup Ivl < sup IfI ~ 188 III (2.30) 2 The Initial-value Problem for Second-order Linear Parabolic Equations (b) Show that for a fixedfECo"'(IR), (kA';; 1/2 and (x,t)E~ lu(x,t)-v(x,t)1 =O(h4). Show that for the special value A= 1/6 the better estimate lu(x,t)-v(x,t)1 =O(h6) holds. [Hint: Expand Au by Taylor's theorem, using u/ = uxx .] (c) Let O<A';; 1/2 and ~Y be the lattice corresponding to h=2- Y, k=A2- 2Y, and let v Y be the corresponding solution of (2.29) with initial valuesf. Let U be the union of the ~Y for v = 1,2,3, .... Show that for (x, t) E U lim vY(x,t)=u(x,t) p--->oo (2.31) provided f has bounded continuous derivatives of orders .;; 4. [Hint: Use the theorem on p. 187 and known properties of u.] (d) Show that (2.31) holds assuming only that O<A';; 1/2 and that f(x) is continuous and has compact support. [Hint: Approximate f uniformly by functions with bounded derivatives of orders .;; 4; use the maximum principle for the v'.] 189 Bibliography [1] Agmon, Shmuel, Lectures on elliptic boundary value problems, Van Nostrand, 1965. [2] Bers, Lipman, John, F., Schechter, M., Partial Differential Equations, Interscience Publishers, 1964. [3] Bremermann, Hans, Distributions, Complex Variables and Fourier Transforms, Addison Wesley Publishers, 1965. [4] Carrier, G. F., and Pearson, C. E., Partial Differential Equations, Academic Press, 1976. [5] Carroll, R c., Abstract Methods in Partial Differential Equations, Harper and Row, 1969. [6] Courant, R, and Friedrichs, K. 0., Supersonic Flow and Shock Waves, 1948, (Repr.), Springer-Verlag. [7] Courant, R., and Hilbert, D., Methods of Mathematical Physics, Interscience Publishers, Vol. I, 1953; Vol. II, 1962. [8] Dunford, N. and Schwartz, J. T., Linear Operators, Part II, Interscience Publishers, 1963. [9] Epstein, B., Partial Differential Equations, McGraw Hill, 1962. [10] Fichera, Gaetano, Linear Elliptic Differential Systems and Eigenvalue Problems, Lecture Notes in Mathematics, 8, Springer-Verlag, 1965. [11] Friedman, Avner, Partial Differential Equations of Parabolic Type, Prentice Hall, 1964. [I2] Friedman, Avner, Partial Differential Equations, Holt, Rinehart and Winston, 1969. [13] Garabedian, P. R, Partial Differential Equations, John Wiley & Sons, Inc., 1964. 191 Bibliography [14] Hellwig, G., Partial Differential Equations, New York, Blaisdell, 1964. [15] Hormander, Lars, Linear Partial Differential Operators, Springer-Verlag, 1963. [16] Isaacson, E., and Keller, H. B., Analysis of Numerical Methods, John Wiley & Sons, Inc., 1966. [17] John, Fritz, Plane Waves and Spherical Means Applied to Partial Differential Equations, Interscience Publishers, 1955. [18] John, Fritz, Lectures on Advanced Numerical Methods, Gordon and Breach, 1967. [19] Lax, P. D., Lectures on Hyperbolic Partial Differential Equations, Stanford University, 1963. [20] Lions, J. L., Equations differentieles operationelles et problemes aux limites, Springer, 1961. [21] Lions, J. L., and Magenes, E., Non-homogeneous boundary value problems, Springer-Verlag, 1972. [22] Mikhlin, S. G., Linear Equations of Mathematical Physics, Holt; Rinehart and Winston, 1967. [23] Petrovsky, I. G., Lectures on Partial Differential Equations, Interscience Publishers, 1954. [24] Protter, M. H. and Weinberger, H. F., Maximum Principles in Differential Equations, Prentice Hall, 1967. [25] Richtmyer, R. D. and Morton, K. W., Difference Methods for Initial Value Problems, 2nd Ed., Interscience Publishers, 1967. [26] Smimov, V. I., A Course of Higher Mathematics, Vol. IV, Translation, Addison Wesley, 1964. [27] Tikhonov, A. N. and Arsenin, V. Y., Solution of Ill-Posed Problems, Winston/Wiley, 1977. [28] Tikhonov, A. N. and Samarskii, A. A., Equations of Mathematical Physics, Translation, Pergamon Press, 1963. [29] Treves, F., Basic Linear Partial Differential Equations, Academic Press, 1975. [30] Widder, D. V., The Heat Equation, Academic Press, 1975. 192 Glossary IR = set of real numbers lIl"=real n-dimensional space (usually endowed with euclidean metric) n c IRn define: n= closure of n For a set an = boundary of n ninl = interior of n wen is compact in n if wis a closed and bounded subset of ninl. For a function j with domain nclRn define: suppj=support of j= closure of subset of n wherej=;eO.fhas compact support in n ifj=O outside a closed and bounded subset of n inl (that is, if j vanishes in a neighborhood of an and outside some ball.) For n c IRn define: Co(n) = set of functions j continuous in n CS(n) = set of j with continuous derivatives of orders ~s in n Co(n) n CS(ninl) = set of j continuous in the closure of n and with continuous derivatives or orders ~s in the interior. CO(n) = set of j with continuous derivatives of orders compact support in n. ~s in n and of For a matrix a = (aik) aT = transpose of a = matrix b = (bik ) = (aki) obtained by interchanging rows and columns of a. a> 0, if aT = a and the quadratic form ~ aik~i~k is positive definite i,k O-notation: u= O(v) if there exists a real constant K such that all pairs u, v under consideration. lui ~Kv for multiple-index notation: see pp.52- 53. ~ = Laplacian '2. a2/ ax? D = d'Alambertian = 0 2 / at 2 - ~ 193 Index A priori estimates 143 Adjoint operator 65, 157 Adjoint problem 66 Amplitude 167 Analytic 173 Analytic function 2 Approximate solution 113, Il8 Arithmetic mean 77 Arrow of time 166, 182 Attraction 81 Autonomous 9 Autonomous system 21 Average 103 Cauchy problem 10, II, 12, 13, 14, 23, 26,29,31,32,54,59,60,75,76, Il2, 113, 132 ClIuchy-Riemann equations 2,80 Cauchy-Schwarz inequalty 149 Cauchy sequence 172 Backward characteristic 46 Backward characteristic cone 114 Backward difference quotients 7 Barrier functions 92 Barrier postulate ·92 Beltrami equation 36 Bessel function III Biharmonic equation 3, 80 Binomial theorem 53 Blow-up 17 Bounded functional 95 Canonical form 46 Cauchy data 32, 33, 55, 59, 113 Cauchy for the quasi-linear equation Cauchy formula 53 Cauchy inequalities 95 Cauchy integral 125 Cauchy-Kowalewski theorem 59 95 Cauchy theorem 80 Cauchy's representation for derivatives 10 Characteristic 32, 55, 58, 59 Characteristic, backward 46 Characteristic curves 9, 10, 13, 18,21,23, 33, 34, 36, 45, 59 Characteristic differential 45 Characteristic direction 9, 10, 19 Characteristic elements 24, 28 Characteristic equations 22 Characteristic form 56 Characteristic hypersurface 166 Characteristic line 4 Characteristic manifolds 52, 58 Characteristic matrix 56, 57 Characteristic projections 13, 59 Characteristic strip 22, 23, 24, 26, 28 Characteristic surfaces 55,57, 58 Characteristics 13, 31, 36, 39 Compact support 67 Compactness 87 Compatibility conditions 31,32,41, 55 Completeness 87, 95, 160 Conductivity coefficient 166 Conjugate harmonic 2,80,81 Connected 83 Conoid 29 Conservation law 17 195 Index Consistency conditions 118, 119, 180 Contractive 47 Correctly-set problems 131 Courant-Friedrichs-Lewy test 6, 7, 8, 184 Courant-Lax theory 44 D'Alembertian 103 Darboux's equation 104 Data 11 Decay 109, 167 Descent 110 Difference equation 5, 182 Difference quotients 151 Differencing a product 151 Differentiation operator 53 Diffusion 166 Dirac function 68 Direction numbers 9, 19 Dirichlet integral 96, 102 Dirichlet norm 97 Dirichlet principle 102 Dirichlet problem 73, 81, 82, 84-102, 132, 160, 163, 164 Dirichlet problem, weak solution of 164 Discontinuity 34 Distribution 68, 70, 75 Distribution solutions 67, 69 Distributions 69 Disturbances 40 Divergence form 17 Divided difference operators 147 Domain of dependence 5,6, 39, 107, 108, III, 113, 119, 155 Domain of influence 115 Duhamel's principle 112, 120 Eigenfunctions 42, 102, II 7 Eigenvalue 102, 117 Elastic equilibrium 159 waves 3, 110, 133 Element(s) 22,24,26,28 characteristic 24 line 23 Elliptic equations 33, 36, 58, 83, 156, 163 Energy 44 estimates 151 identity 73, 140 inequality 139, 141 integral 116, 119 norm 107 Envelopes 20, 28 Euler-Lagrange equations 30 Euler-Poisson-Dabroux equation 105 Euler's P.D.E. for homogeneous functions 15 Extremal property 89 Extremals 30 196 Finite differences, method of 146, 181 First-order equation 1 systems 44, 139 Flow 2 Focussing 106, 109 Form canonical 46 characteristic 56 divergence 17 normal 36 standard 60 Fourier formula 168 transform 122 transformation 122, 162, 168 Functional 67 bounded 96 linear 95 Fundamental solution(s) 70, 74, 75, 79, 80, 84, 137, 157, 159, 160, 164 for the Laplace equation 159 with pole 69 Garding's hyperbolicity condition 125, 128, 133, 145 inequality 160, 164 strong inequality 165 Gauss divergence theorem 64 Gauss's law of the arithmetic mean 77 General solution 10 Generalized solutions 33, 40, 67 Geometric optics 26 Gradient catastrophe 17 Gradient 52 Gravitational attraction 80 Green's function 84, 88 identities 72, 142 Hadamard's method of descent 110 Hamilton-Jacobi equation 30 Harmonic 75, 76, 77, 83, 87, 88 conjugate 2, 80, 81 functions 2, 75, 76, 86 Harnack's inequality 88 Heat conduction 3 distribution 174 equation 3, 166, 168, 174, 177, 179 Hilbert space 94,95, WI, 160 Hodograph method 37 Holmgren's theorem 66, 129, 146 Homogeneous function 15 system of equations 164 Index Huygens's construction 30, 107 principle in the strong form 108, 111 Hyperbolic 33, 36, 38, 45, 122 equations 103, 120 second-order equation 139 strictly 129, 136 symmetric 145 Hyperbolicity 58, 128, 129 Improperly posed problems 131 Incorrectly set problems 131 Influence 5, 40, 107 Initial boundary value problems 40, 116 conditions 120 curve 23 data 139 functions 39 value problem 11, 39, 45, 103, 120, 145, 166, 170, 185 value problem for the wave equation 106 values 4, 11 velocity distribution 16 Inner product space 95 Instability 6 Integral 22 surface 19, 23, 24, 28, 29 Integration by parts 64 Irreversible 166 Jump 17, 34, 35 condition 18 intensity 35 Korteweg-deVries equation 4 Lagrange-Green identity 64, 65, 67, 69 Lame constants 3 Laplace equation 2,72,73,75,76,78, 159 operator 2, 58, 65, 72 Lattice 153, 182 Lax-Milgram le=a 160, 164 Legendre transformation 37 Level lines 27 Line element 23 Linear equation 1, 13, 54 first-order system 57 functional 95 parabolic equations 181 second-order equation 35 Liouville's theorem 88 Lorentz transformation 116 Lower boundary 174, 188 Majorise 61,62,63, 173 Maximum norm 47,182 principle 81, 82, 83, 88, 170, 174, 181, 183 Maxwell's equation 2 Mean value property 77,79 Mesh ratio 7 Minimal surface 3, 37 Mixed initial-boundary-value problems 48, 119, 133, 179 Modified Dirichlet problem 94 Monge cone 19,20,26,29 Monomial 52 Multi-index 52 Navier-Stokes equations 4 Neumann problem 73, 81 Newton's law 80 Noncharacteristic 55, 56, 57, 113 Norm 160 equivalent 162 maximum 182 Normal derivative 32 distance 28 form 36 Operator adjoint 65, 157 divided difference 147 Laplace 2, 58, 65, 72 shift 6, 147 Order 1 O.D.E. 9 Pailey-Wiener theorem 129 Parabolic 33, 36 Parallel curves 28 Parseval's identity 144, 162 Perron's method 89 Phase lag 167 Plane element 22 wave function 135, 136, 157, 159 Poincare inequality 97, 102, 163 Poisson's differential equation 78 formula 77, 88, 99, 100, 160, 169 integral formula 84, 85, 88 kernel 85 Polytropic gas 3 Potential 81 functions 2 theory 73 velocity 2, 3 Principal part 56, 57, 128 Propagating waves 38 197 Index Propagation 23 of discontinuity 35 of singularities 33, 58 speed of . 131 Pure initial-value problem 43, 48 Quasi-linear equations 1, 8, 18 systems 48, 50 Radon-problem 138 transformation 138 Ray 23,27 Real analytic 53, 160 Reduced wave operator 79 Reflection 76, 84, 88, 180 Regularity 75, 177 Representation theorem 96 Round-off errors 6, 8 Schrodinger's wave equation 3 Schwartz notation 54 Second-order equation 31 Selfadjoint 75 Separation of variables 42 Shift operators 6, 147 Shock condition 17 Signals 40 Simple wave 50 Smooth 171 Sobolev inequalities 144, 146, 152 Solution approximate 113, 118 distribution 69 fundamental 69, 70, 74, 75, 79, 80, 84, 137, 157, 159, 160 general 10 generalized 33 strict 34, 143 weak 17, 69, 40, 141 Space-like 27, 114, 115, 119, 122, 132, . 146 Speed of propagation 18, 131 Spherical means 103, 104 synunetry 73, 79, 80, 109 Stability 7, 147, 183 Standard form of the initial-value problem 60, 120, 129, 131, 137 Strict solution 34, 143 Strictly hyperbolic 129, 136 Strip 26 characteristic 22, 23, 24, 26 condition 22, 23, 31 Strongly elliptic 165 Subharmonic 77, 79, 83, 89 Symbol 56, 57 198 Symmetric hyperbolic 139, 140, 145 System autonomous 21 first order 139 of equations 164 of first order equations 44 quasi-linear 48 undetermined 21 Telegraph equation III Temperature distribution 166, 167 Test function 67, 69, 157 Theta-function 180 Time-like 27, 115 Triangle inequalities 95 Tricomi equation 36 Tychonoff solution 171, 176 Type .33 Undetermined system 21 Unique continuation 53 Uniqueness 12 for the initial value problem theorem of Holmgren 65 145, 176 Variational problem 30 Vector space 94 Velocity field 16 potential 2, 3 Vibration of string 44 Water waves 2,4 Wave fronts 26, 27 operator 79 propagating 5 Wave equation 38, 106, 121, 133, 138, 146 homogeneous 112 in 5 dimensions 109 in n-dimensional space 103, 127 in 3 dimensions 138 inhomogeneous 112 initial problem for the 132 standard problem for the 127 Wavelength 167 Waves circular 30 elastic 3, 110 plane 135, 157, 159 propagating 38 simple 50 water 2,4 Weak solutions 17, 18, 40, 141, 160, 164 Weierstrass's approximation theorem 173 Well-posed problems 131, 132