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Du Jun,Yu Zhihao.Numerical study of rapid cyclogenesis over sea[J].Acta Oceanologica Sinica,1989,(1):51-62
Numerical study of rapid cyclogenesis over sea
Numerical study of rapid cyclogenesis over sea
投稿时间:1987-07-06  修订日期:1987-11-10
DOI:
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英文关键词:
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作者单位
Du Jun Department of Atmospheric Sciences, Nanjing University, Nanjing, China 
Yu Zhihao Department of Atmospheric Sciences, Nanjing University, Nanjing, China 
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中文摘要:
      A five-layer primitive equation model was used in the study of rapid cyclogenesis over sea. The numerical simulations show that the Tibetan Plateau, large-scale baroclinicity and heat flux from the sea surface are the three important agents to produce cyclonic vorticity along the east coast of China. The diagnostic computation of a 24 h control simulation indicates that the nonlinear vorticity advection, baroclinicity and diabatic heating are also responsible for the development of the extratropical cyclones over seas.
英文摘要:
      A five-layer primitive equation model was used in the study of rapid cyclogenesis over sea. The numerical simulations show that the Tibetan Plateau, large-scale baroclinicity and heat flux from the sea surface are the three important agents to produce cyclonic vorticity along the east coast of China. The diagnostic computation of a 24 h control simulation indicates that the nonlinear vorticity advection, baroclinicity and diabatic heating are also responsible for the development of the extratropical cyclones over seas.
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