| “海棠”台风风浪场分析 |
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| 引用本文： | 吴晓峰,于芸,邓小东,徐丽丽.“海棠”台风风浪场分析[J].海洋预报,2009,26(3):86-92. |
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| 作者姓名： | 吴晓峰 于芸 邓小东 徐丽丽 |
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| 作者单位： | 国家海洋局东海预报中心,上海,200081 |
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| 摘 要： | 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.
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| 关 键 词： | 台风 风区 风时 风浪 涌浪 |
Characteristic analysis of wind waves induced by Typhoon Haitang (0505) |
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| WU Xiao-feng,YU Yun,DENG Xiao-dong,XU Li-li.Characteristic analysis of wind waves induced by Typhoon Haitang (0505)[J].Marine Forecasts,2009,26(3):86-92. |
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| Authors: | WU Xiao-feng YU Yun DENG Xiao-dong XU Li-li |
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| Institution: | Marine Forecast Center of East China Sea;Shanghai 200081 China |
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| Abstract: | 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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| Keywords: | typhoon wind fetch wind duration wind wave swell |
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