80 research outputs found

    On the striated regularity for the 2D anisotropic Boussinesq system

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    In this paper, we investigate the global existence and uniqueness of strong solutions to 2D Boussinesq system with anisotropic thermal diffusion or anisotropic viscosity and with striated initial data. Using the key idea of Chemin to solve 2-D vortex patch of ideal fluid, namely the striated regularity can help to bound the gradient of the velocity, we can prove the global well-posedness of the Boussinesq system with anisotropic thermal diffusion with initial vorticity being discontinuous across some smooth interface. In the case of an anisotropic horizontal viscosity we can study the propagation of the striated regularity for the smooth temperature patches problem.Comment: 36 page

    Global unique solvability of inhomogeneous Navier-Stokes equations with bounded density

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    In this paper, we prove the global existence and uniqueness of solution to d-dimensional (for d=2,3d=2,3) incompressible inhomogeneous Navier-Stokes equations with initial density being bounded from above and below by some positive constants, and with initial velocity u0∈Hs(R2)u_0\in H^s(\R^2) for s>0s>0 in 2-D, or u0∈H1(R3)u_0\in H^1(\R^3) satisfying |u_0|_{L^2}|\na u_0|_{L^2} being sufficiently small in 3-D. This in particular improves the most recent well-posedness result in [10], which requires the initial velocity u0∈H2(Rd)u_0\in H^2(\R^d) for the local well-posedness result, and a smallness condition on the fluctuation of the initial density for the global well-posedness result

    Global well-posedness of 33-D anisotropic Navier-Stokes system with small unidirectional derivative

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    In \cite{LZ4}, the authors proved that as long as the one-directional derivative of the initial velocity is sufficiently small in some scaling invariant spaces, then the classical Navier-Stokes system has a global unique solution. The goal of this paper is to extend this type of result to the 3-D anisotropic Navier-Stokes system (ANS)(ANS) with only horizontal dissipation. More precisely, given initial data u_0=(u_0^\h,u_0^3)\in \cB^{0,\f12}, (ANS)(ANS) has a unique global solution provided that |D_\h|^{-1}\pa_3u_0 is sufficiently small in the scaling invariant space $\cB^{0,\f12}.

    Global regularity for some classes of large solutions to the Navier-Stokes equations

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    In three previous papers by the two first authors, classes of initial data to the three dimensional, incompressible Navier-Stokes equations were presented, generating a global smooth solution although the norm of the initial data may be chosen arbitrarily large. The main feature of the initial data considered in the last paper is that it varies slowly in one direction, though in some sense it is ``well prepared'' (its norm is large but does not depend on the slow parameter). The aim of this article is to generalize the setting of that last paper to an ``ill prepared'' situation (the norm blows up as the small parameter goes to zero).The proof uses the special structure of the nonlinear term of the equation
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