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A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION
作者姓名:杨波  钱永甫
作者单位:Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008;Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008
基金项目:This paper was jointly supported by the National Key Ptoject of Fundamental Research, Climate Dynamics and Theoretical Study on Climate Predictability and the National Natural Science Foundation of China.
摘    要:A two-layer primitive equation model is developed in this paper. The capabilities of this model aretested by the use of multiyearly averaged January and July sea surface level pressure fields and windfields which can be diagnosed from the pressure fields. The results show that the ocean surface currentsand undercurrents in the second layer driven by the sea surface wind and the sea surface pressure areclose to the observation. The results are also compared with that of the IAP OGCM and the OSUOGCM.

关 键 词:ocean  circulation  model  numerical  simulations
收稿时间:7/3/1995 12:00:00 AM
修稿时间:3/6/1996 12:00:00 AM

A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION
Yang Bo and Qian Yongfu.A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION[J].Journal of Tropical Meteorology,1997,3(1):85-94.
Authors:Yang Bo and Qian Yongfu
Institution:Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008;Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008
Abstract:A two-layer primitive equation model is developed in this paper. The capabilities of this model aretested by the use of multiyearly averaged January and July sea surface level pressure fields and windfields which can be diagnosed from the pressure fields. The results show that the ocean surface currentsand undercurrents in the second layer driven by the sea surface wind and the sea surface pressure areclose to the observation. The results are also compared with that of the IAP OGCM and the OSUOGCM.
Keywords:ocean circulation model  numerical simulations
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