Asymptotic solution of a weak nonlinear model for the mid-latitude stationary wind field of a two-layer barotropic ocean

A weak nonlinear model of a two-layer barotropic ocean with Rayleigh dissipation is built.The analytic asymptotic solution is derived in the mid-latitude stationary wind field,and the physical meaning of the corresponding problem is discussed.

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Bibliographic Details
Published inChinese physics B Vol. 22; no. 3; pp. 72 - 78
Main Author 林万涛 张宇 莫嘉琪
Format Journal Article
LanguageEnglish
Published 01.03.2013
Subjects
Asymptotic properties
Dissipation
Freshwater
Mathematical analysis
Mathematical models
Nonlinearity
Oceans
中纬度
正压
海洋
渐近解
物理意义
非线性模型
风场
Online AccessGet full text
ISSN1674-1056
2058-3834
1741-4199
DOI10.1088/1674-1056/22/3/030205

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Summary:A weak nonlinear model of a two-layer barotropic ocean with Rayleigh dissipation is built.The analytic asymptotic solution is derived in the mid-latitude stationary wind field,and the physical meaning of the corresponding problem is discussed.
Bibliography:A weak nonlinear model of a two-layer barotropic ocean with Rayleigh dissipation is built.The analytic asymptotic solution is derived in the mid-latitude stationary wind field,and the physical meaning of the corresponding problem is discussed.
two-layer barotropic ocean,ocean model asymptotic solution
11-5639/O4
Lin Wan-Tao , Zhang Yu , Mo Jia-Qi（1） state Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029, China ;2） University of the Chinese Academy of Sciences, Beijing 100049, China ;3 ）Department of Mathematics, Anhui Normal University, Wuhu 241003, China
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SourceType-Scholarly Journals-1
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content type line 23
ISSN:1674-1056
2058-3834
1741-4199
DOI:10.1088/1674-1056/22/3/030205