| 长涂岛的台风暴潮 |
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| 引用本文： | 林传兰.长涂岛的台风暴潮[J].海洋学研究,1991,9(3):12-19. |
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| 作者姓名： | 林传兰 |
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| 作者单位： | 国家海洋局第二海洋研究所 杭州，310012 |
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| 摘 要： | 本文根据1968～1981年台风期间的水位观测资料,对长涂岛的台风暴潮特性及影响因子作了统计研究。结果表明,1、长涂岛的台风暴潮主要发生在7～9月间,大于100cm的最大增水较少发生;2、台风过程最大增水与台风路径的关系密切,较大的台风暴潮发生在台风接近时;3、台风过程增水与岱山气象站(相距15km)的气压有较好的负相关。而与风速有较好的正相关;4、台风过程最大增水与天文潮高潮相遇并非罕见。
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| 关 键 词： | 长涂岛 台风暴潮 |
Typhoon surge of the changtu Island |
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| Lin Chuanlan.Typhoon surge of the changtu Island[J].Journal of Marine Sciences,1991,9(3):12-19. |
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| Authors: | Lin Chuanlan |
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| Abstract: | In this paper, based on the observations during the period from 1968 to 1981, typhoon surge characteristics of the Changtu Island and influence factors are analysed using statistical and correlation methods. The results are as follows: (1) typhoon surges of the island occur from July to September, and surges of higher than 120cm are rare; (2) the highest typhoon surge is closely related to the paths of typhoon; (3) there are the higher negative correlation between typhoon surges and pressure of Daishan , While the higher positive correlation between typhoon surges and wind speeds of Daishan; and (4) typhoon surges encounter highest tide of astronomical tides are not rare. |
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| Keywords: | Changtu Island typhoon surge |
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