| 海燕台风与冷高压共同作用对温台沿海潮位的影响及成因探讨 |
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| 引用本文： | 朱忠良,薛志刚.海燕台风与冷高压共同作用对温台沿海潮位的影响及成因探讨[J].海洋预报,2002,19(3):53-58. |
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| 作者姓名： | 朱忠良 薛志刚 |
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| 作者单位： | 1. 温州海洋预报台,温州
2. 温州市防汛办,温州 |
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| 摘 要： | 2001年10月产生的台风海燕引起了温台沿海较高潮位。本文通过对台风与冷高压共同作用机制的探讨，主要从沿海梯度风的变化分析这次风暴潮造成的高水位，从而为秋季冷空气影响期间的风暴潮预报积累经验。
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| 关 键 词： | 沿海潮位 成因 台风 冷高压 温州市 台州市 风暴潮 |
| 文章编号： | 1003-0239(2002)-03-0053-06 |
THE JOINT EFFECT OF TYPHOON HAIYAN AND COLD HIGH PRESSURE ON THE COASTAL TIDAL LEVEL OF WENZHOU AND TAIZHOU AND ITS RESEARCH |
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| Zhu Zhongliang.THE JOINT EFFECT OF TYPHOON HAIYAN AND COLD HIGH PRESSURE ON THE COASTAL TIDAL LEVEL OF WENZHOU AND TAIZHOU AND ITS RESEARCH[J].Marine Forecasts,2002,19(3):53-58. |
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| Authors: | Zhu Zhongliang |
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| Abstract: | The typhoon Haiyan produced in October, 2001 caused a relatively high tidal level of Wenzhou and Taizhou coastal area. The article shows that joint effect mechanism of typhoon itself and cold high pressure, was the formation cause of high tidal level It will be helpful to accumulate experience of storm surge forecasting during the cold air affecting period. |
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| Keywords: | typhoon cold high pressure high tidal level research |
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