2,305 research outputs found

    On the cubic NLS on 3D compact domains

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    We prove bilinear estimates for the Schr\"odinger equation on 3D domains, with Dirichlet boundary conditions. On non-trapping domains, they match the R3\mathbb{R}^3 case, while on bounded domains they match the generic boundary less manifold case. As an application, we obtain global well-posedness for the defocusing cubic NLS for data in H0s(Ω)H^s_0(\Omega), 1<s31<s\leq 3, with Ω\Omega any bounded domain with smooth boundary.Comment: 15 pages, updated references and corrected typos. To appear in Journal of the Institute of Mathematics of Jussie

    On uniqueness for the critical wave equation

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    We prove the uniqueness of weak solutions to the critical defocusing wave equation in 3D under a local energy inequality condition. More precisely, we prove the uniqueness of uL_t(H˙1)W˙1,_t(L2) u \in L^\infty\_t(\dot{H}^{1})\cap \dot{W}^{1,\infty}\_t(L^2), under the condition that uu verifies some local energy inequalities.Comment: 12 pages, to appear in Comm. Partial Differential Equation

    On well-posedness for the Benjamin-Ono equation

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    We prove existence of solutions for the Benjamin-Ono equation with data in Hs(R)H^s(\R), s>0s>0. Thanks to conservation laws, this yields global solutions for H12(R)H^\frac 1 2(\R) data, which is the natural ``finite energy'' class. Moreover, inconditional uniqueness is obtained in Lt(H12(R))L^\infty_t(H^\frac 1 2(\R)), which includes weak solutions, while for s>320s>\frac 3 {20}, uniqueness holds in a natural space which includes the obtained solutions.Comment: Important changes. We improved both existence and uniqueness results. In particular, uniqueness holds in the natural Lt;Hx1/2L^\infty_t; H^{1/2}_x energy spac

    Transport of gaussian measures by the flow of the nonlinear Schr\"odinger equation

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    We prove a new smoothing type property for solutions of the 1d quintic Schr\"odinger equation. As a consequence, we prove that a family of natural gaussian measures are quasi-invariant under the flow of this equation. In the defocusing case, we prove global in time quasi-invariance while in the focusing case because of a blow-up obstruction we only get local in time quasi-invariance. Our results extend as well to generic odd power nonlinearities.Comment: Presentation improve

    Dispersion for the wave equation inside strictly convex domains I: the Friedlander model case

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    We consider a model case for a strictly convex domain of dimension d2d\geq 2 with smooth boundary and we describe dispersion for the wave equation with Dirichlet boundary conditions. More specifically, we obtain the optimal fixed time decay rate for the smoothed out Green function: a t1/4t^{1/4} loss occurs with respect to the boundary less case, due to repeated occurrences of swallowtail type singularities in the wave front set.Comment: 53 pages, 4 figures, to appear in Annals of Math. Fixed typos, added remark

    A profile decomposition approach to the L∞/t (L3/ x) Navier–Stokes regularity criterion

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    In this paper we continue to develop an alternative viewpoint on recent studies of Navier–Stokes regularity in critical spaces, a program which was started in the recent work by Kenig and Koch (Ann Inst H Poincaré Anal Non Linéaire 28(2):159–187, 2011). Specifically, we prove that strong solutions which remain bounded in the space L3(R3) do not become singular in finite time, a known result established by Escauriaza et al. (Uspekhi Mat Nauk 58(2(350)):3–44, 2003) in the context of suitable weak solutions. Here, we use the method of “critical elements” which was recently developed by Kenig and Merle to treat critical dispersive equations. Our main tool is a “profile decomposition” for the Navier–Stokes equations in critical Besov spaces which we develop here. As a byproduct of this tool, assuming a singularity-producing initial datum for Navier–Stokes exists in a critical Lebesgue or Besov space, we show there is one with minimal norm, generalizing a result of Rusin and Sverak (J Funct Anal 260(3):879–891, 2011)

    Le transfert d'échelle

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