| 台风动力模式的解析解及台风形成和维持的动力机制(二) |
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| 引用本文： | 李小凡. 台风动力模式的解析解及台风形成和维持的动力机制(二)[J]. 热带气象学报, 1987, 0(4): 338-345 |
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| 作者姓名： | 李小凡 |
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| 作者单位： | 上海台风研究所 |
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| 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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| 收稿时间： | 1986-04-03 |
| 修稿时间： | 1987-02-03 |
ANALYTIC SOLUTIONS OF DYNAMIC MODEL AND DYNAMIC MECHANISM OF THE FORMATION AND MAINTENANCE OF TYPHOON(PART: II) |
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| Li Xiaofan. ANALYTIC SOLUTIONS OF DYNAMIC MODEL AND DYNAMIC MECHANISM OF THE FORMATION AND MAINTENANCE OF TYPHOON(PART: II)[J]. Journal of Tropical Meteorology, 1987, 0(4): 338-345 |
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| Authors: | Li Xiaofan |
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| Affiliation: | 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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