| 摘要: |
| 本文是文献[1]的继续。采用轴对称的动力方程组对台风中层对流层和边界层两个区域求得解析解,利用得到的结果讨论了台风形成和维持的动力机制;在边界层采用海气耦合方程组计算发现,高海温中心区有利于台风边界层低压扰动的加深。 |
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| ANALYTIC SOLUTIONS OF DYNAMIC MODEL AND DYNAMIC MECHANISM OF THE FORMATION AND MAINTENANCE OF TYPHOON(PART: II) |
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Li Xiaofan
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Shanghai Typhoon Institute
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| Abstract: |
| This is discussion continuing from paper I. Analytic solutions of mid-troposphere and boundary layer of typhoon are obtained by using axis-symmetric dynamic equations, and dynamic mechanisms of the formation and maintenance of typhoon are discussed by utilizing the results. Furthermore, It is found that high sea-surface temperature area is useful to deepen the typhoon depression by using the sea -air coupled equations in boundary layer. |
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