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Qiao Fangli,Zhang Qinghua,He Wen. 1996. An analytical diagnostic model of the Antarctic Circumpolar Current. Acta Oceanologica Sinica, (1):9-17
An analytical diagnostic model of the Antarctic Circumpolar Current
An analytical diagnostic model of the Antarctic Circumpolar Current
Received:November 10, 1995  Revised:November 30, 1995
DOI:
Key words:Antarctic Circumpolar Current  quasi-geostrophic vorticity equation  basic balance
中文关键词:  Antarctic Circumpolar Current  quasi-geostrophic vorticity equation  basic balance
基金项目:The project was supported by National Natural Science Foundation of China.
Author NameAffiliation
Qiao Fangli The project was supported by National Natural Science Foundation of China 
Zhang Qinghua The project was supported by National Natural Science Foundation of China 
He Wen The project was supported by National Natural Science Foundation of China 
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Abstract:
      Based on a linear quasi-geostrophic vorticity equation, we have set up an analytical diagnostic mode for the Antarctic Circumpolar Current.The results, how that the balance among wind stress, ocean horizontal viscous stress and the p-effect is the basic balance of the Antarctic Circumpolar Current, and the center velocity of the jet, coming from the Drake Passage, will decrease due to the ocean dynamic adjustment, and the width in the north-south direction will decrease gradually.The jet coming from the Drake Passage moves about 4° northward because of the inducement of winddriven currents.The clockwise vorticity appearing in the south-west comer corresponds to the Wedded Gyre.The characters of the Antarctic Circumpolar Current described by the model are congruous with observations basically.
中文摘要:
      Based on a linear quasi-geostrophic vorticity equation, we have set up an analytical diagnostic mode for the Antarctic Circumpolar Current.The results, how that the balance among wind stress, ocean horizontal viscous stress and the p-effect is the basic balance of the Antarctic Circumpolar Current, and the center velocity of the jet, coming from the Drake Passage, will decrease due to the ocean dynamic adjustment, and the width in the north-south direction will decrease gradually.The jet coming from the Drake Passage moves about 4° northward because of the inducement of winddriven currents.The clockwise vorticity appearing in the south-west comer corresponds to the Wedded Gyre.The characters of the Antarctic Circumpolar Current described by the model are congruous with observations basically.
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