The primitive equations approximation of the anisotropic horizontally viscous 3D Navier-Stokes equations

Abstract. In this paper, we provide rigorous justification of the hydrostatic approximation and the derivation of primitive equations as the small aspect ratio limit of the incompressible three-dimensional Navier-Stokes equations in the anisotropic horizontal viscosity regime. Setting ε > 0 to be the small aspect ratio of the vertical to the horizontal scales of the domain, we investigate the case when the horizontal and vertical viscosities in the incompressible three-dimensional Navier-Stokes equations are of orders O(1) and O(ε), respectively, with α > 2, for which the limiting system is the primitive equations with only horizontal viscosity as ε tends to zero. In particular we show that for “well prepared” initial data the solutions of the scaled incompressible threedimensional Navier-Stokes equations converge strongly, in any finite interval of time, to the corresponding solutions of the anisotropic primitive equations with only horizontal viscosities, as ε tends to zero, and that the convergence

[1]  L. E. Fraenkel,et al.  NAVIER-STOKES EQUATIONS (Chicago Lectures in Mathematics) , 1990 .

[2]  G. Vallis Atmospheric and Oceanic Fluid Dynamics: Fundamentals and Large-Scale Circulation , 2017 .

[3]  A vertical diffusion model for lakes , 1999 .

[4]  Existence of a strong solution and trajectory attractor for a climate dynamics model with topography effects , 2018 .

[5]  Boling Guo,et al.  Existence of weak solutions and trajectory attractors for the moist atmospheric equations in geophysics , 2006 .

[6]  I. Kukavica,et al.  On the regularity of the primitive equations of the ocean , 2007 .

[7]  J. Lions,et al.  New formulations of the primitive equations of atmosphere and applications , 1992 .

[8]  E. Titi,et al.  Strong solutions to the 3D primitive equations with only horizontal dissipation: near $H^1$ initial data , 2016, 1607.06252.

[9]  Francisco Guillén,et al.  Mathematical Justification of the Hydrostatic Approximation in the Primitive Equations of Geophysical Fluid Dynamics , 2001, SIAM J. Math. Anal..

[10]  Jinkai Li,et al.  Existence and Uniqueness of Weak Solutions to Viscous Primitive Equations for a Certain Class of Discontinuous Initial Data , 2015, SIAM J. Math. Anal..

[11]  Y. Giga,et al.  The hydrostatic approximation for the primitive equations by the scaled Navier–Stokes equations under the no-slip boundary condition , 2020, Journal of Evolution Equations.

[12]  E. Titi,et al.  Local Well-Posedness of Strong Solutions to the Three-Dimensional Compressible Primitive Equations , 2018, Archive for Rational Mechanics and Analysis.

[13]  E. Titi,et al.  Global well‐posedness and finite‐dimensional global attractor for a 3‐D planetary geostrophic viscous model , 2003 .

[14]  E. Titi,et al.  The primitive equations as the small aspect ratio limit of the Navier–Stokes equations: Rigorous justification of the hydrostatic approximation , 2017, Journal de Mathématiques Pures et Appliquées.

[15]  Daiwen Huang,et al.  On the 3D viscous primitive equations of the large-scale atmosphere , 2009 .

[16]  Y. Giga,et al.  The primitive equations in the scaling-invariant space L∞(L1)\documentclass[12pt]{minimal} \usepackage{amsmath} \usepackage{wasysym} \usepackage{amsfonts} \usepackage{amssymb} \usepackage{amsbsy} \usepackage{mathrsfs} \usepackage{upgreek} \setlength{\oddsidemargin}{-69pt} \begin{document}$$L^{\infty , 2017, Journal of Evolution Equations.

[17]  Edriss S. Titi,et al.  On the Effect of Rotation on the Life-Span of Analytic Solutions to the 3D Inviscid Primitive Equations , 2020, Archive for Rational Mechanics and Analysis.

[18]  E. Titi,et al.  Global Well‐Posedness of the Three‐Dimensional Primitive Equations with Only Horizontal Viscosity and Diffusion , 2016 .

[19]  Michele Coti Zelati,et al.  The equations of the atmosphere with humidity and saturation: Uniqueness and physical bounds , 2013 .

[20]  E. Titi,et al.  Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics , 2005, math/0503028.

[21]  M. Wrona,et al.  Primitive equations with horizontal viscosity: The initial value and The time-periodic problem for physical boundary conditions , 2019, Discrete & Continuous Dynamical Systems.

[22]  Roger Temam,et al.  Mathematical theory for the coupled atmosphere-ocean models (CAO III) , 1995 .

[23]  J. Holton Geophysical fluid dynamics. , 1983, Science.

[24]  E. Titi,et al.  Finite-Time Blowup for the Inviscid Primitive Equations of Oceanic and Atmospheric Dynamics , 2012, 1210.7337.

[25]  Takahito Kashiwabara,et al.  Global strong Lp well-posedness of the 3D primitive equations with heat and salinity diffusion , 2016, 1605.02614.

[26]  Q. Jiu,et al.  Global existence of weak solutions to 3D compressible primitive equations with degenerate viscosity , 2020 .

[27]  E. Titi,et al.  Finite-time blowup and ill-posedness in Sobolev spaces of the inviscid primitive equations with rotation , 2020, 2009.04017.

[28]  E. Titi,et al.  Local and Global Well-Posedness of Strong Solutions to the 3D Primitive Equations with Vertical Eddy Diffusivity , 2013, 1312.6035.

[29]  E. Titi,et al.  Global Well–Posedness of the 3D Primitive Equations with Partial Vertical Turbulence Mixing Heat Diffusion , 2010, Communications in Mathematical Physics.

[30]  E. Titi,et al.  Global well-posedness of the 3D primitive equations with horizontal viscosity and vertical diffusivity , 2017, Physica D: Nonlinear Phenomena.

[31]  Takahito Kashiwabara,et al.  Global Strong Well-Posedness of the Three Dimensional Primitive Equations in $${L^p}$$Lp-Spaces , 2015, 1509.01151.

[32]  E. Titi,et al.  Global well-posedness for the primitive equations coupled to nonlinear moisture dynamics with phase changes , 2019, Nonlinearity.

[33]  A. Majda Introduction to PDEs and Waves in Atmosphere and Ocean , 2003 .

[34]  A. V. Kazhikhov,et al.  Existence of a Global Solution to One Model Problem of Atmosphere Dynamics , 2005 .

[35]  T. Wong Blowup of Solutions of the Hydrostatic Euler Equations , 2012, 1211.0113.

[36]  Edriss S. Titi,et al.  Global Existence of Weak Solutions to the Compressible Primitive Equations of Atmospheric Dynamics with Degenerate Viscosities , 2018, SIAM J. Math. Anal..

[37]  Q. Jiu,et al.  Uniqueness of the global weak solutions to 2D compressible primitive equations , 2017 .

[38]  I. Kukavica,et al.  Primitive equations with continuous initial data , 2014 .

[39]  G. Kobelkov,et al.  Existence of a solution ‘in the large’ for the 3D large-scale ocean dynamics equations , 2006 .

[40]  E. Titi,et al.  Global well-posedness for passively transported nonlinear moisture dynamics with phase changes , 2016, 1610.00060.

[41]  Hantaek Bae Navier-Stokes equations , 1992 .

[42]  E. Titi,et al.  Global Well-posedness of Strong Solutions to the 3D Primitive Equations with Horizontal Eddy Diffusivity , 2014, 1401.1234.

[43]  W. Washington,et al.  An Introduction to Three-Dimensional Climate Modeling , 1986 .

[44]  Roger Temam,et al.  On the equations of the large-scale ocean , 1992 .

[45]  Y. Giga,et al.  The hydrostatic Stokes semigroup and well-posedness of the primitive equations on spaces of bounded functions , 2018, Journal of Functional Analysis.

[46]  Y. Giga,et al.  Rigorous justification of the hydrostatic approximation for the primitive equations by scaled Navier–Stokes equations , 2018, Nonlinearity.

[47]  B. Han,et al.  Global well–posedness for the 3D primitive equations in anisotropic framework , 2020 .

[48]  Hongjun Gao,et al.  On the Hydrostatic Approximation of Compressible Anisotropic Navier–Stokes Equations–Rigorous Justification , 2020, Journal of Mathematical Fluid Mechanics.

[49]  N. Ju On $H^2$ solutions and $z$-weak solutions of the 3D Primitive Equations , 2015, 1507.06685.

[50]  R. Temam,et al.  Navier-Stokes equations: theory and numerical analysis: R. Teman North-Holland, Amsterdam and New York. 1977. 454 pp. US $45.00 , 1978 .