中国物理B ›› 2013, Vol. 22 ›› Issue (3): 30205-030205.doi: 10.1088/1674-1056/22/3/030205

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

林万涛a, 张宇b, 莫嘉琪c   

  1. a State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics,Chinese Academy of Sciences, Beijing 100029, China;
    b University of the Chinese Academy of Sciences, Beijing 100049, China;
    c Department of Mathematics, Anhui Normal University, Wuhu 241003, China
  • 收稿日期:2012-07-18 修回日期:2012-08-16 出版日期:2013-02-01 发布日期:2013-02-01
  • 基金资助:
    Project supported by the National Key Development Program for Basic Research of China (Grant No. 2011CB403501) and the National Natural Science Foundation of China (Grant Nos. 41175058, 41275062, and 11202106).

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

Lin Wan-Tao (林万涛)a, Zhang Yu (张宇)b, Mo Jia-Qi (莫嘉琪)c   

  1. a State Key Laboratory of Numerical Modeling for Atmospheric Sciences and Geophysical Fluid Dynamics, Institute of Atmospheric Physics,Chinese Academy of Sciences, Beijing 100029, China;
    b University of the Chinese Academy of Sciences, Beijing 100049, China;
    c Department of Mathematics, Anhui Normal University, Wuhu 241003, China
  • Received:2012-07-18 Revised:2012-08-16 Online:2013-02-01 Published:2013-02-01
  • Contact: Lin Wan-Tao E-mail:linwt@lasg.iap.ac.cn
  • Supported by:
    Project supported by the National Key Development Program for Basic Research of China (Grant No. 2011CB403501) and the National Natural Science Foundation of China (Grant Nos. 41175058, 41275062, and 11202106).

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

关键词: twolayer barotropic ocean, ocean model asymptotic solution

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

Key words: two-layer barotropic ocean, ocean model asymptotic solution

中图分类号:  (Sequences, series, and summability)

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