| 莱州湾风暴潮的形成与增水量评估 |
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| 引用本文： | 山义昌,张芹,杨付津,赵春生.莱州湾风暴潮的形成与增水量评估[J].山东气象,2006,26(4):4-5. |
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| 作者姓名： | 山义昌 张芹 杨付津 赵春生 |
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| 作者单位： | 1. 潍坊市气象局,山东,潍坊,261011
2. 昌邑市气象局,山东,昌邑,261300 |
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| 基金项目： | 山东省潍坊市科技局风暴潮的规律与预报研究课题(wy05163)资助 |
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| 摘 要： | 运用昌邑市下营水文站和寿光市羊口水文站的资料,对莱州湾风暴潮的形成机制和影响系统进行了分析.结果发现:诱发莱州湾风暴潮的天气系统主要有热带气旋、温带气旋及冷锋.由于莱州湾特殊的地理构造和地形条件,风暴潮在爆发过程中,有3个比较明显的天气机制,即爆发前的东南大风、爆发中的东北大风及其持续时间、天文大潮.对风暴潮各阶段的增水量值进行了定量的估计.
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| 关 键 词： | 莱州湾 风暴潮 机制 |
| 文章编号： | 1005-0582(2006)04-0004-02 |
| 修稿时间： | 2006年6月23日 |
The Formation of the Storm Surge and the Assesment of Tidewfater in Laizhou Bay |
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| SHAN Yi-chang,ZHANG Qin,YANG Fu-jin,ZHAO Chun-sheng.The Formation of the Storm Surge and the Assesment of Tidewfater in Laizhou Bay[J].Journal of Shandong Meteorology,2006,26(4):4-5. |
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| Authors: | SHAN Yi-chang ZHANG Qin YANG Fu-jin ZHAO Chun-sheng |
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| Abstract: | Using data from Xiaying hydrological station in Changyi county and Yangkou hydrological station in Shouguang county,the influencing systems of the storm surge in Laizhou Bay is analysed.The results show:The main weather systems causing storm surge can be divided into three categories:Temperate cyclone;Tropical cyclone;Cold front.Because of the special geographic structure and landform,the formation mechanism of the storm surge is as follows.The early strong southeast wind;Continual strong northeast wind during it bursting;The high chronometric tide.Some meaning to forecast storm surge in Laizhou Bay is found. |
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| Keywords: | Laizhou bay storm surge mechanism |
| 本文献已被 CNKI 维普 万方数据 等数据库收录！ |
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