| Du Jun,Yu Zhihao. 1989. Numerical study of rapid cyclogenesis over sea. Acta Oceanologica Sinica, (1):51-62 |
| Numerical study of rapid cyclogenesis over sea |
| Numerical study of rapid cyclogenesis over sea |
| Received:July 06, 1987 Revised:November 10, 1987 |
| DOI: |
| Key words: |
| 中文关键词: |
| 基金项目: |
|
| Hits: 1887 |
| Download times: 684 |
| Abstract: |
| 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. |
| 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. |
|
HTML
View Full Text
View/Add Comment Download reader |
| Close |