Strong solutions to the 3D primitive equations with only horizontal dissipation: Near H1 initial data

被引:55
作者
Cao, Chongsheng [1 ]
Li, Jinkai [2 ]
Titi, Edriss S. [3 ,4 ]
机构
[1] Florida Int Univ, Dept Math, Univ Pk, Miami, FL 33199 USA
[2] Chinese Univ Hong Kong, Dept Math, Shatin, Hong Kong, Peoples R China
[3] Texas A&M Univ, Dept Math, 3368 TAMU, College Stn, TX 77843 USA
[4] Weizmann Inst Sci, Dept Comp Sci & Appl Math, IL-76100 Rehovot, Israel
关键词
Primitive equations; Anisotropic dissipation; Planetary oceanic and atmospheric; model; GLOBAL WELL-POSEDNESS; LARGE-SCALE OCEAN; ATMOSPHERE; REGULARITY; EXISTENCE; BLOWUP; HEAT;
D O I
10.1016/j.jfa.2017.01.018
中图分类号
O1 [数学];
学科分类号
0701 ; 070101 ;
摘要
In this paper, we consider the initial boundary value problem of the three-dimensional primitive equations for oceanic and atmospheric dynamics with only horizontal viscosity and horizontal diffusivity. We establish the local, in time, well-posedness of strong solutions, for any initial data (v(0), T-0) is an element of H-1, by using the local, in space, type energy estimate. We also establish the global well-posedness of strong solutions for this system, with any initial data (v(0), T-0) is an element of H-1 boolean AND L-infinity such that partial derivative(z)v(0) is an element of, for some m is an element of (2, infinity), by using the logarithmic type anisotropic Sobolev inequality and a logarithmic type Gronwall inequality. This paper improves the previous results obtained in Cao et al. (2016) [10], where the initial data (v(0), T-0) was assumed to have H-2 regularity. (C) 2017 Elsevier Inc. All rights reserved.
引用
收藏
页码:4606 / 4641
页数:36
相关论文
共 48 条
  • [1] [Anonymous], 1988, Chicago Lectures in Mathematics
  • [2] [Anonymous], 1986, Annali di Matematica Pura ed Applicata, DOI [DOI 10.1007/BF01762360.MR916688, DOI 10.1007/BF01762360]
  • [3] [Anonymous], PREPRINT
  • [4] [Anonymous], 1969, Mathematics and Its Applications
  • [5] Mathematical justification of the hydrostatic approximation in the primitive equations of geophysical fluid dynamics
    Azérad, P
    Guillén, F
    [J]. SIAM JOURNAL ON MATHEMATICAL ANALYSIS, 2001, 33 (04) : 847 - 859
  • [6] STABILITY OF TWO-DIMENSIONAL VISCOUS INCOMPRESSIBLE FLOWS UNDER THREE-DIMENSIONAL PERTURBATIONS AND INVISCID SYMMETRY BREAKING
    Bardos, C.
    Lopes Filho, M. C.
    Niu, Dongjuan
    Nussenzveig Lopes, H. J.
    Titi, E. S.
    [J]. SIAM JOURNAL ON MATHEMATICAL ANALYSIS, 2013, 45 (03) : 1871 - 1885
  • [7] Bresch D., 2003, Differ. Integral Equ., V16, P77
  • [8] Brezis H., 1980, Nonlinear Analysis Theory, Methods & Applications, V4, P677, DOI 10.1016/0362-546X(80)90068-1
  • [9] Brezis H., 1980, COMMUN PART DIFF EQ, V5, P773, DOI 10.1080/03605308008820154
  • [10] Global well-posedness of the three-dimensional viscous primitive equations of large scale ocean and atmosphere dynamics
    Cao, Chongsheng
    Titi, Edriss S.
    [J]. ANNALS OF MATHEMATICS, 2007, 166 (01) : 245 - 267