| A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION |
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| 引用本文： | 杨波,钱永甫. A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION[J]. 热带气象学报(英文版), 1997, 3(1): 85-94 |
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| 作者姓名： | 杨波 钱永甫 |
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| 作者单位： | Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008;Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008 |
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| 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. |
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| 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.
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| 关 键 词： | ocean circulation model numerical simulations |
| 收稿时间： | 1995-07-03 |
| 修稿时间： | 1996-03-06 |
A TWO-LAYER PRIMITIVE EQUATION OCEAN CURRENT MODEL AND ITS SIMULATION |
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| 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 |
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| Authors: | Yang Bo and Qian Yongfu |
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| Affiliation: | Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008;Dapartment of Atmospheric Sciences, Nanjing University, Nanjing, 210008 |
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| 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. |
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| Keywords: | ocean circulation model numerical simulations |
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