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

被引:60
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
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