Characteristics Analysis and Risk Assessment of Extreme Water Levels Based on 60-Year Observation Data in Xiamen, China
Characteristics Analysis and Risk Assessment of Extreme Water Levels Based on 60-Year Observation Data in Xiamen, China作者机构:National Marine Data and Information ServiceTianjin 300171China Shandong Province Key Laboratory of Ocean EngineeringOcean University of ChinaQingdao 266100China
出 版 物:《Journal of Ocean University of China》 (中国海洋大学学报(英文版))
年 卷 期:2022年第21卷第2期
页 面:315-322页
核心收录:
学科分类:07[理学] 0707[理学-海洋科学] 08[工学] 0816[工学-测绘科学与技术]
基 金:supported by the National Key Research and Development Program of China(No.2016YFC1401103) the NSFC-Shandong Joint Foundation(No.U1706226) the National Natural Science Foundation of China(No.51779236) the Open Fund of Shandong Province Key Laboratory of Ocean Engineering(No.kloe201903)
主 题:storm surge astronomical tide extreme water level hazard risk
摘 要:Extreme water levels are related to astronomical tides and storm *** typhoon systems,which have caused extreme water level rises,were selected based on 60-yr water level data from the Xiamen tide gauge *** these 11 typhoon systems,the astronomical tide component accounts for 71%-95%of the total water *** Gumbel distribution of extreme water level rise was estimated,and the impact of typhoon surges on water levels during the return period was *** ex-treme tide levels caused by typhoons Herb(1996)and Dujuan(2015)are much higher than those of other typhoons and correspond to the return period of 76 yr and 71 yr,*** differences of sea levels in the presence and absence of these two typhoons in the 10-100 yr return period are 5.8-11.1 *** the 100-yr return period,the total risks within 10,25,50,and 100 yr increase by 94.3%,85.4%,72.9%,and 54.4%,respectively,if the Herb and Dujuan are not *** that typhoon Herb(1996)occurred during the highest astronomical tide,it will produce a water level higher than that of the 1000-yr return *** level rise has an important influence on the water level return period,and the contribution of nonlinear sea level rise in the next 100 yr is estimated to be 10.34%.