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Effects of tide-surge interactions on storm surges along the coast of the Bohai Sea, Yellow Sea, and East China Sea

Effects of tide-surge interactions on storm surges along the coast of the Bohai Sea, Yellow Sea, and East China Sea

作     者:XU JunLi ZHANG YuHong CAO AnZhou LIU Qiang LV XianQing 

作者机构:Key Laboratory of Physical Oceanography (Ocean University of China) Ministry of Education Ocean University of China College of Engineering Ocean University of China 

出 版 物:《Science China Earth Sciences》 (中国科学(地球科学英文版))

年 卷 期:2016年第59卷第6期

页      面:1308-1316页

核心收录:

学科分类:07[理学] 0707[理学-海洋科学] 

基  金:provided by the National Natural Science Foundation of China(Grant No.41371496) the National Science and Technology Support Program(Grant No.2013BAK05B04) the Natural Science Foundation of Shandong Province of China(Grant No.ZR2014DM017) the Opening Fund of Shandong Provincial Key Laboratory of Marine Ecology and Environment&Disaster Prevention and Mitigation(Grant No.201411) the Applied Research Fund for Postdoctoral Researchers of Qingdao(Grant No.82214263) 

主  题:Storm surges Astronomical tides Tide-surge interactions Typhoon 7203 Coupled tide-surge model 

摘      要:A two-dimensional coupled tide-surge model was used to investigate the effects of tide-surge interactions on storm surges along the coast of the Bohai Sea, Yellow Sea, and East China Sea. In order to estimate the impacts of tide-surge interactions on storm surge elevations, Typhoon 7203 was assumed to arrive at 12 different times, with all other conditions remaining constant. This allowed simulation of tide and total water levels for 12 separate cases. Numerical simulation results for Yingkou, Huludao, Shijiusuo, and Lianyungang tidal stations were analyzed. Model results showed wide variations in storm surge elevations across the 12 cases. The largest difference between 12 extreme storm surge elevation values was of up to 58 cm and occurred at Yingkou tidal station. The results indicate that the effects of tide-surge interactions on storm surge elevations are very significant. It is therefore essential that these are taken into account when predicting storm surge elevations.

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