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台风“利奇马”对渤海风暴潮影响研究
作者:李健1 2 3 4  侯一筠1 2 3 5  刘清容4  姜涛6  焦艳4 
单位:1. 中国科学院海洋研究所, 山东 青岛 266071;
2. 中国科学院海洋环流与波动重点实验室, 山东 青岛 266071;
3. 中国科学院大学, 北京 100049;
4. 国家海洋局北海预报中心, 山东 青岛 266061;
5. 青岛海洋科学与技术试点国家实验室海洋动力过程与气候功能实验室,
关键词:台风“利奇马” 渤海 台风风暴潮 FVCOM 
分类号:P731.23
出版年·卷·期(页码):2021·38·第一期(34-42)
摘要:
利用实测资料对比和FVCOM数值模拟等方法,研究了“利奇马”台风风暴潮在渤海的演变规律。研究表明:渤海沿岸的风暴潮过程是由局地风“直接作用”及外部天气系统“间接影响”共同作用引起的,且它们引起的风暴潮时空分布明显不同。在“利奇马”台风风暴潮中,“直接作用”引起的风暴增水在渤海湾和莱州湾沿岸分别约占总风暴增水的2/3和1/2。
In this paper, the evolution mechanism of the storm surge caused by typhoon "Likima" in the Bohai Sea is studied based on the in-situ observation data and FVCOM. The results show that the storm surge in the Bohai Sea is jointly caused by direct-effect of local wind and indirect-effect of the marginal weather system with different spatial and temporal distribution. For the storm surge caused by typhoon "Lekima", the direct-effect accounts for 2/3 and 1/2 of the total storm surge in the Bohai Bay and Laizhou Bay, respectively.
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