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

作　　者：林万涛 张宇 莫嘉琪 

机构地区：[1]State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics,Institute of Atmospheric Physics, Chinese Academy of Sciences [2]University of the Chinese Academy of Sciences [3]Department of Mathematics,Anhui Normal University

出　　处：《Chinese Physics B》2013年第3期72-78,共7页中国物理B（英文版）

基　　金：Project supported by the National Basic Research Program of China (Grant No. 2011CB403501);the National Natural Science Foundation of China (GrantNos. 41175058,41275062,and 11202106)

摘　　要：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.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.

关 键 词：two-layer barotropic ocean ocean model asymptotic solution 

分 类 号：P732[天文地球—海洋科学]