ebook img

The periodic b-equation and Euler equations on the circle PDF

0.13 MB·English
Save to my drive
Quick download
Download
Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.

Preview The periodic b-equation and Euler equations on the circle

THE PERIODIC b-EQUATION AND EULER EQUATIONS ON THE CIRCLE JOACHIM ESCHER ANDJO¨RG SEILER Abstract. In thisnote weshow that theperiodic b-equationcan only 0 berealizedasanEulerequationontheLiegroupDiff∞(S1)ofallsmooth 1 and orientiation preserving diffeomorphisms on the cirlce if b = 2, i.e. 0 for the Camassa-Holm equation. In this case the inertia operator gen- 2 eratingthemetriconDiff∞(S1)isgivenbyA=1−∂x2. Incontrast,the Degasperis-Procesi equation, for which b = 3, is not an Euler equation n a on Diff∞(S1) for any inertia operator. Our result generalizes a recent J result of B. Kolev [24]. 8 1 ] P 1. Introduction A In this note we are interested in the geometric interpretation of the so- . h called b-equation t a (1) m = −(m u+bmu ), t ∈ R, x ∈ S1, t x x m with the momentum variable m given by [ m = u−u , 1 xx v and where b stands for a real parameter, cf. [13, 12, 19]. It was shown in 7 8 [13, 19, 26, 20] that equation (1) is asymptotically integrable, a necessary 9 condition for complete integrability, but only for the values b = 2 and b = 3. 2 In case b = 2 we recover the Camassa-Holm equation (CH) . 1 (2) u −u +3uu −2u u −uu = 0, 0 t txx x x xx xxx 0 while for b = 3 we obtain the Degasperis-Procesi equation (DP) 1 : v ut−utxx+4uux−3uxuxx−uuxxx = 0. i X Independent of (asymptotical) integrability, equation (1) possesses some r hydrodynamic relevance, as described for instance in [22, 21, 11]. Each of a these equations models the unidirectional irrotational free surface flow of a shallow layer ofaninviscidfluidmovingundertheinfluenceof gravity over a flatbed. Inthesemodels,u(t,x)representsthewave’s heightatthemoment t and at position x above the flat bottom. The periodic Camassa-Holm equation is known to correspond to the geo- desic flow with respect to the metric induced by the inertia operator 1−∂2 x on the diffeomorphism group of the circle, cf. [25]. Local existence of the geodesics and properties of the Riemannian exponential map were studied in [9, 10]. The whole family of b-equations and in particular (DP) can be 2000 Mathematics Subject Classification. 35Q53, 58D05. Key words and phrases. Euler equation, diffeomorphisms group of the circle, Degasperis-Procesi equation. 1 2 J.ESCHERANDJ.SEILER realized as (in general) non-metric Euler equations, i.e. as geodesic flows with respect to a linear connection which is not necessarily Riemannian in the sense that there may not exist a Riemannian metric which is preserved by this connection, cf. [15]. Besides various common properites of the individual members of the b- equation, there are also significant differences to report on. It is known that solutions of the CH-equation preserve the H1-norm in time and that (CH) possesses global in time weak solutions, cf. [7, 5, 3]. In particular there are no shock waves for (CH), although finite time blow of classical solutions occurs, but in form of wave breaking: solutions to (CH) stay continuous and bounded but their slopes may blow up in finite time, cf. [6, 8]. Wave breaking is also observed for the (DP) but in a weaker form. It seems that the H1-norm of solutions of (DP) cannot be uniformly bounded, but L∞- boundsfor large classes of initital values are available [16, 17, 18]. Moreover shock waves, i.e. discontinuous global travelling wave soltions are known to exist. Indeed it was shown in [14] that sinh(x−[x]−1/2) u (t,x) = , x ∈ R/Z, c tcosh(1/2)+csinh(1/2) is for any c > 0 a global weak solution to the (DP) equation. In this note we disclose a further difference between the (CH) and the (DP) equation, by proving that in a fairly large class of Riemannian metrics on Diff∞(S1) it is impossible to realize (DP) as a geodesic flow. The note is organized as follows. In Section 2, we first introduce the concept geodesic flows and Euler equations on a general Lie group. Subse- quently, in Section 3, the important special case of Diff∞(S1) is discussed and Section 4 contains the proof of our main result. 2. The Euler equation on a general Lie group In his famous article [1] Arnold established a deep geometrical connection between the Euler equations for a perfect fluid in two and three dimensions and thegeodesic flow for right-invariant metrics on theLie group of volume- preservingdiffeomorphisms. After Arnold’s fundamental work a lot of effort wasdevotedtounderstandthegeometricstructureofotherphysicalsystems with a Lie group as configuration space. The general Euler equation was derived initially for the Levi-Civita con- nection of aone-sided invariant Riemannian metricon aLiegroup G(see [1] or [2]) butthe theory is even valid in the more general setting of a one-sided invariant linear connection, see [15]. A right invariant metric on a Lie group G is determined by its value at theunitelement e of the group, i.e. by an innerproducton its Liealgebra g. Thisinner productcan beexpressed in terms of a symmetric linear operator ∗ A :g → g , i.e. hAu,vi = hAv,ui, for all u, v ∈ g, ∗ ∗ whereg isthedualspaceofgandh·,·idenotestheduality pairingong ×g. ∗ Each symmetric isomorphism A :g → g is called an inertia operator on G. The corresponding metric on G induced by A is denoted by ρ . A THE PERIODIC b-EQUATION AND EULER EQUATIONS ON THE CIRCLE 3 Let ∇ denote the Levi-Civita connection on G induced by ρ . Then A 1 (3) ∇ ξ = [ξ ,ξ ]+B(ξ ,ξ ), ξu v 2 u v u v where ξ is the right invariant vector field on G, generated by u ∈g. More- u over, [·,·] is the Lie bracket on Vect(G), the smooth sections of the tangent bundle over G, and the bilinear operator B is called Christoffel operator. It is defined by the following formula 1 ∗ ∗ (4) B(u,v) = (ad ) (v)+(ad ) (u) , u v 2h i ∗ where (ad ) is the adjoint with respect to ρ of the natural action of g on u A itself, given by (5) ad : g → g, v 7→ [u,v]. u A proof of the above statments as well as of the following proposition can be found in [15]. Proposition 1. A smooth curve g(t) on a Lie group G is a geodesic for a right invariant linear connection ∇ defined by (3) iff its Eulerian velocity u= g′◦g−1 satisfies the first order equation (6) u = −B(u,u). t Equation (6) is known as the Euler equation. 3. The Euler equation on Diff∞(S1) Since the tangent bundle TS1 ≃ S1 × R is trivial, Vect∞(S1), the space of smooth vector fields on S1, can be identified with C∞(S1), the space of real smooth functions on S1. Furthermore, the group Diff∞(S1) is naturally equipped with a Fr´echet manifold structure modeled over C∞(S1), cf. [15]. The Lie bracket on Vect∞(S1)≃ C∞(S1) is given by1 [u,v] = u v−uv . x x The topological dual space of Vect∞(S1) ≃ C∞(S1) is given by the dis- tributions Vect′(S1) on S1. In order to get a convenient representation of the Christoffel operator B we restrict ourselves to Vect∗(S1), the set of all regular distributions which may be represented by smooth densities, i.e. T ∈ Vect∗(S1) iff there is a ̺ ∈C∞(S1) such that hT,ϕi = ̺ϕdx for all ϕ∈ C∞(S1). Z S1 By Riesz’ representation theorem we may identify Vect∗(S1) ≃ C∞(S1). InthefollowingwedenotebyLsym(C∞(S1))thesetofallcontinuousisomor- is phisms on C∞(S1), which are symmetric with respect to the L (S1) inner 2 product. Definition 2. Each A ∈ Lsym(C∞(S1)) is called a regular inertia operator is on Diff∞(S1). 1Notice that this bracket differs from theusual bracket of vector fields bya sign. 4 J.ESCHERANDJ.SEILER Proposition 3. Given A ∈ Lsym(C∞(S1)), we have that is 1 B(u,v) = A−1[2Au·v +2Av·u +u·(Av) +v·(Au) ] x x x x 2 for all u, v ∈ C∞(S1). Proof. Let u, v, w ∈ C∞(S1) be given. Recalling (5), integration by parts yields ∗ ρ ((ad ) v,w) = ρ (v,ad w) = Av·(u w−uw )dx A u A u Z x x S1 = [(Av)u +((Av)·u) ]wdx. x x Z S1 This shows that ∗ (ad ) v = 2(Av)u +u(Av) . u x x Symmetrization of this formula completes the proof, cf. (4). (cid:3) Examples 4. It may be instructive to discuss two paradigmatic examples. (1) First we choose A= id. Then B(u,u) = −3uu and the correspond- x ing Euler equation u +3uu = 0 is known as the periodic inviscid t x Burgers equation, see e.g. [4, 23]. (2) Next we choose A = id − ∂2. Then the Euler equation reads as x u = −(1−∂2)−1(3uu −2u u −uu ), which equivalent to the t x x x xx xxx periodic Camassa-Holm equation, cf. (2). 4. The family of b-equations Each A ∈ Lsym(C∞(S1)) induces an Euler equation on Diff∞(S1). Con- is versely, given b ∈ R, we may ask whether there exists a regular inertia operator such that the b-equation is the corresponding Euler equation on Diff∞(S1). We know from Example 4.2 that the answer is positive if b = 2. The following result shows that the answer is negative if b 6= 2. Theorem 5. Let b ∈ R be given and suppose that there is a regular inertia operator A∈ Lsym(C∞(S1)) such that the b-equation is m = −(m u+bmu ), m = u−u t x x xx is the Euler equation on Diff∞(S1) with respect to ρ . Then b = 2 and A A= id−∂2. x Corollary 6. The Degasperis-Procesi equation m = −(m u+3mu ), m = u−u t x x xx cannot be realized as an Euler equation for any regular inertia operator A∈ Lsym(C∞(S1)). is Proof of Theorem 5. Let b ∈ R be given and assume that the b-equation is the Euler equation on Diff∞(S1) with respect to ρ . Letting L = 1−∂2, we A x then get (7) A−1 2(Au)u +u(Au) = L−1 b(Lu)u +u(Lu) x x x x (cid:16) (cid:17) (cid:16) (cid:17) for all u ∈C∞(S1). THE PERIODIC b-EQUATION AND EULER EQUATIONS ON THE CIRCLE 5 (a) Let 1 denote the constant function with value 1. Choosing u = 1 in (7), we get A−1(1(A1) ) = 0 and hence (A1) = 0, i.e. A1 is constant. x x Scaling (7), we may assume that A1 = 1. Next we replace u by u+λ in (7). Then we find for the left-hand side that 1 A−1 2 A(u+λ) (u+λ) +(u+λ) A(u+λ) λ (cid:16) x x(cid:17) (cid:0) (cid:1) (cid:0) (cid:1) 1 = A−1 2 (Au)+λ u +(u+λ)(Au) x x λ (cid:16) (cid:17) (cid:0) (cid:1) 2(Au)u +u(Au) =A−1 x x +2u +(Au) x x (cid:16) λ (cid:17) −λ−→−∞→ A−1 2u +(Au) , x x (cid:0) (cid:1) and similarly for the right-hand side: 1 L−1 b L(u+λ) (u+λ) +(u+λ) L(u+λ) λ (cid:16) x x(cid:17) (cid:0) (cid:1) (cid:0) (cid:1) −λ−→−∞→ L−1 bu +(Lu) . x x (cid:0) (cid:1) Combing these limits, we conclude that (8) A−1 2u +(Au) = L−1 bu +(Lu) x x x x (cid:0) (cid:1) (cid:0) (cid:1) for all u ∈C∞(S1). Setting u = einx, we find that n L−1 b(u ) +(Lu ) = iα u , n x n x n n (cid:0) (cid:1) where α := n+ bn/(1+n2) . Applying A to (8) with u = u thus yields n n (cid:0) (cid:1) 2inu +(Au ) = iα Au . n n x n n Therefore v := Au solves the ordinary differential equation n n ′ (9) v −iα v = −2inu . n n For n 6= 0, let us solve (9) explicitly. Assume first that b = 0. Then v(x) = (c−2inx)u n for some constant c. But this function is never 2π-periodic. Thus we must have b 6= 0. However, in this case (10) v = Au =γ eiαnx+β u (n 6= 0) n n n n n 2(1+n2) with β = and suitable constants γ . n b n (b) Assume that all γ vanish, i.e. Au = β u for all n 6= 0 and A1= 1. n n n n Inparticular,AisaFouriermultiplication operatorandthuscommuteswith L. Therefore we can write (7) as L 2(Au)u +u(Au) = A b(Lu)u +u(Lu) . x x x x (cid:16) (cid:17) (cid:16) (cid:17) Inserting u= u a direct computation yields n 3(1+4n2)β = (1+b)(1+n2)β . n 2n Using that β = 2(1+n2)/b, this is equivalent to b = 2. Then β = 1+n2 n n and therefore A coincides with L. 6 J.ESCHERANDJ.SEILER (c) Let us assume there is a p ∈ Z\{0} such that γ 6= 0. We shall derive p a contradiction. Since v = Au must be 2π-periodic, α is an integer. This p p p implies that b = k(1+p2)/p for some non-zero integer k. We set (11) m := α . p Observe that m 6= p, since b 6= 0. Thus (u |u ) = 0 and (10) implies that p m L2 (Au |u ) = (γ eimx|u ) = γ . p m L2 p m L2 p By the symmetry of A we also find that γ = (Au |u ) = (u |Au ) = γ (u |eiαmx) . p p m L2 p m L2 m p L2 Since γ 6= 0 we must have γ 6= 0. Again by periodicity we conclude that p m α ∈ Z. But then α = p, since otherwise we would have (u |eiαmx) = 0 m m p L2 and thus again γ = 0. We know already that b = k(1 + p2)/p. Thus p m = α = p+k by (11) and the definition α . Now we calculate p p p+k p = α = α = p+k+b m p+k 1+(p+k)2 k(1+p2) p+k = p+k+ · , p 1+(p+k)2 and we find p 1+(p+k)2 k+k(1+p2)(p+k) = 0. (cid:0) (cid:1) Observing that k 6= 0, an elementary calculation yields (12) 2p3+3p2k+pk+2p+k = 0. From this we conclude that there is an l ∈ Z such that k = pl. With this we infer from (12) that (l+2) (l+1)p2 +1 = 0. (cid:0) (cid:1) The only integer solution of this equation is l = −2. In fact, the solution l = − 1 −1 is only possible if p2 = 1 and thus again l = −2, since for p2 6= 1 p2 we have l 6∈Z. Therefore b = −2(1+p2) and thus α = −p. p Moreover, we can conclude that γ = 0 whenever n6= 0 does not coincide n with p or −p, since otherwise the same calculation as before would show b = −2(1+n2) contradicting b = −2(1+p2). Now insert u= u in (7). The left-hand side then equals p 3ip A−1 ipγ 1−3ipu = ipγ 1− u ; p 2p p 2p (cid:16) (cid:17) β2p for the latter identity note that 2p does not coincide with p or −p, so that γ = 0, and hence A−1u = u /β . Note also that β = −1. For the 2p 2p 2p 2p p right-hand side we get p(1+p2) i(1+b) u . 1+4p2 2p Comparing both expressions we conclude that pγ = 0 which is a contradic- p tion to p 6= 0 and γ 6= 0. (cid:3) p THE PERIODIC b-EQUATION AND EULER EQUATIONS ON THE CIRCLE 7 References 1. V.I.Arnold,Surlag´eom´etriediff´erentielledesgroupes deLiededimensioninfinieet sesapplications`al’hydrodynamiquedesfluidesparfaits,Ann.Inst.Fourier(Grenoble) 16 (1966), no. fasc. 1, 319–361. MR 0202082 2. V. I. Arnold and B. Khesin, Topological methods in hydrodynamics, Applied Mathe- matical Sciences, vol. 125, Springer-Verlag, New York,1998. MR 1612569 3. A. Bressan and A. Constantin, Global conservative solutions of the Camassa-Holm equation, Arch.Rational Mech. Anal.183 (2007), 215–239. MR 2278406 4. J. M. Burgers, A mathematical model illustrating the theory of turbulence, Advances inAppliedMechanics,AcademicPressInc.,NewYork,N.Y.,1948,editedbyRichard von Mises and Theodore von K´arma´n,, pp.171–199. MR 0027195 5. A. Constantin and J. Escher, Global weak solutions for a shallow water equation, Indiana Univ.Math. J. 47 (1998), 1527–1546. MR 1687106 6. , Wave breaking for nonlinear nonlocal shallow water equations, Acta Math. 181 (1998), no. 2, 229–243. MR 1668586 7. ,Well-posedness, globalexistence, andblowupphenomena foraperiodic quasi- linear hyperbolic equation, Comm. Pure Appl. Math. 51 (1998), no. 5, 475–504. MR 1604278 8. ,Ontheblow-uprateandtheblow-upsetofbreakingwavesforashallowwater equation, Math. Z. 233 (2000), no. 1, 75–91. MR 1738352 9. A. Constantin and B. Kolev, On the geometric approach to the motion of inertial mechanical systems, J. Phys.A 35 (2002), no. 32, R51–R79. MR 1930889 10. , Geodesic flow on the diffeomorphism group of the circle, Comment. Math. Helv. 78 (2003), no. 4, 787–804. MR 2016696 11. A. Constantin and D. Lannes, The hydrodynamical relevance of the Camassa-Holm and Degasperis-Procesi equations, Arch.Ration. Mech. Anal.192 (2009), no. 1, 165– 186. MR 2481064 12. A.Degasperis,D.D.Holm,andA.N.I.Hone,A new integrable equation withpeakon solutions, Teoret. Mat. Fiz. 133 (2002), no. 2, 170–183. MR 2001531 13. A. Degasperis and M. Procesi, Asymptotic integrability, Symmetry and perturbation theory(Rome,1998),WorldSci.Publ.,RiverEdge,NJ,1999,pp.23–37. MR1844104 14. J.Escher,Wavebreakingandshockwavesforaperiodicshallowwaterequation,Philos. Trans. R. Soc. Lond. Ser. A Math. Phys. Eng. Sci. 365 (2007), no. 1858, 2281–2289. MR 2329148 15. J.EscherandKolev,TheDegasperis-Procesi equationasanon-metricEulerequation, preprint, arXiv:0908.0508, 2010. 16. J. Escher, Y. Liu, and Z. Yin, Global weak solutions and blow-up structure for the Degasperis-Procesi equation,J.Funct.Anal.241(2006),no.2,457–485. MR2271927 17. ,Shockwavesandblow-upphenomenafortheperiodicDegasperis-Procesiequa- tion, IndianaUniv.Math. J. 56 (2007), no. 1, 87–117. MR 2305931 18. J. Escher and Z. Yin, Well-posedness, blow-up phenomena, and global solutions for the b-equation, J. ReineAngew. Math. 624 (2008), 51–80. MR 2456624 19. A.N.W.HoneandJ.P.Wang,Prolongation algebras and Hamiltonian operators for peakon equations, InverseProblems 19 (2003), no. 1, 129–145. MR 1964254 20. R.I.Ivanov,Onthe integrability of aclass of nonlinear dispersive waves equations, J. Nonlinear Math. Phys.12 (2005), no. 4, 462–468. MR 2171998 21. , Water waves and integrability, Philos. Trans. R. Soc. Lond. Ser. A Math. Phys. Eng. Sci. 365 (2007), no. 1858, 2267–2280. MR 2329147 22. R. S. Johnson, The classical problem of water waves: a reservoir of integrable and nearly-integrable equations, J. Nonlinear Math. Phys. 10 (2003), no. suppl. 1, 72–92. MR 2063546 23. T. Kato, The Cauchy problem for quasi-linear symmetric hyperbolic systems, Arch. Ration. Mech.Anal. 58 (1975), 181–205. 24. B.Kolev,SomegeometricinvestigationsontheDegasperis-Procesishallowwaterequa- tion, WaveMotion 46 (2009), 412–419. 8 J.ESCHERANDJ.SEILER 25. S. Kouranbaeva, The Camassa-Holm equation as a geodesic flow on the diffeomor- phism group, J. Math. Phys.40 (1999), no. 2, 857–868. MR 1674267 26. A. V. Mikhailov and V. S. Novikov, Perturbative symmetry approach, J. Phys. A 35 (2002), no. 22, 4775–4790. MR 1908645 Institute for Applied Mathematics, University of Hannover, D-30167 Han- nover, Germany E-mail address: [email protected] Department of Mathematical Sciences, Loughborough University, Leices- tershire LE11 3TU, United Kingdom E-mail address: [email protected]

See more

The list of books you might like

Most books are stored in the elastic cloud where traffic is expensive. For this reason, we have a limit on daily download.