| 引用本文： |
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陈波,邱绍芳.广西沿海港湾风暴潮增减水与台风路径和地形效应的关系[J].广西科学,2000,7(4):282-285. [点击复制]
- Chen Bo,Qiu Shaofang.Impacts of Typhoon Course and Land form on Water Level Fluctuation in the Coastal Bays in Guangxi[J].Guangxi Sciences,2000,7(4):282-285. [点击复制]
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| 摘要: |
| 通过资料分析表明,广西沿海港湾风暴潮增减水分布趋势是湾内大,离岸递减。增减水受台风路径和地形效应的影响显著,但不同台风路径和港湾地形引起的风暴潮增减水值差异很大。 |
| 关键词: 风暴潮 增减水 台风路径 地形效应 |
| DOI： |
| 投稿时间：2000-07-12修订日期：2000-09-05 |
| 基金项目:广西自然科学基金资助项目(合同号0009020)。 |
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| Impacts of Typhoon Course and Land form on Water Level Fluctuation in the Coastal Bays in Guangxi |
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Chen Bo, Qiu Shaofang
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| (Guangxi Academy of Sciences, 32 Xinghulu, Nanning, Guangxi, 530022, China) |
| Abstract: |
| According to the recorded historically information of typhoons, the water level fluctuation caused by storm surges in the coastal bays in Guangxi shows a trend of greater inside bays and descending with standing off shore. Typhoon course and landform have great impact on water level fluctuation of the bays, but these impacts are remarkably different between different typhoon courses and between landforms. |
| Key words: storm surge water level fluctuation typhoon course landform |
