On the order of magnitude of the baroclinic flow in the primitive equations of the ocean

被引：6

作者：

Simonnet, E.

Medjo, T. Tachim

Temam, R.

机构：

[1] CNRS, Inst Non Lineaire Nice, F-06560 Valbonne, France

[2] Florida Int Univ, Dept Math, Miami, FL 33199 USA

[3] Indiana Univ, Inst Appl Math & Sci Comp, Bloomington, IN 47405 USA

来源：

ANNALI DI MATEMATICA PURA ED APPLICATA | 2006年 / 185卷 / Suppl 5期

关键词：

primitive equations; geostrophic; asymptotic; barotropic flow; baroclinic flow;

D O I：

10.1007/s10231-004-0146-0

中图分类号：

O29 [应用数学];

学科分类号：

070104 ;

摘要：

In this article, we study the baroclinic flow in the primitive equations (PEs) of the ocean, which are known to be the fundamental equations of the ocean, [4]-[8]. We prove that the magnitude of the baroclinic flow in the L-2-norm is of order O(delta), where delta is the aspect ratio of the ocean. Some numerical simulations of the PEs of the ocean consistent with these estimates are also presented.

引用

页码：S293 / S313

页数：21

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