| “海棠”台风风浪场分析 |
| 作者：吴晓峰 于芸 邓小东 徐丽丽 |
| 单位：国家海洋局东海预报中心 上海 200081 |
| 关键词：台风 风区 风时 风浪 涌浪 |
| 分类号：P444 |
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| 出版年·卷·期（页码）：2009·26·第三期（86-92） |
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摘要：
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| 通过对0505号"海棠"台风的高、低空气流场的分析,揭示了"海棠"台风浪成长、发展、消衰的机制和规律。结果表明:台风浪的大小和范围不仅与台风的强度、移速及周围大尺度天气系统有关,而且也受岛屿及海底地形等环境条件的影响。 |
| Based on the analysis of the lower and upper air flow fields of Typhoon Haitang (0505), the mechanism of evolution, development and downgrade of typhoon-induced wind waves was studied in this paper. It was shown that the magnitude and range of wind waves are not only related to the strength, moving speed and the surrounding large-scale meteorological systems of the typhoon, but also influenced by the island and topography of sea floor. |
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参考文献：
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[1] John Yeung.热带气旋强度研究.香港热带气旋追击站,2002.htt://www.hkcoc.com.
[2] 雷小途.热带气旋的结构对其路径偏折的分析[C],第11届全国热带气旋科学讨论会论文摘要文集.中国气象科学院,1999,58-60.
[3] 包澄澜.海洋灾害及预报[M],海洋出版社,1991,43-44 |
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