东南沿海台风风暴潮特点及其变化规律  

FEATURE AND VARIED RULE OF TYPHOON STORM SURGE ALONG THE COAST OF SOUTH EAST CIIINA SEA

作　　者：刘金芳[1] 郝培章[1] 俞慕耕[1] 江伟[1] 尼建军[1] 

机构地区：[1]海军海洋水文气象中心

出　　处：《海洋预报》2002年第1期81-88,共8页Marine Forecasts

摘　　要：本文收集了１９４９～１９９０年的台风及相应验潮站的实测潮位资料，计算分析了连云 港至汕头之间沿海港口的热带气旋增水，得出了东南沿海各港口的增水特征。该海域风暴潮 强度较大，易形成特大潮灾，各港口最大增水出现时间不一，有的在热带气旋登陆前，有的 在热带气旋登陆后，多数在热带气旋登陆前后０～６ｈ。台凤及风暴潮易造成舰船、码头等损 坏，形成非战斗力减员。In this paper, the tropical cyclone data and the tide data of corresponding tidal observational station during 1949~ 1990 was collected. The features of storm surge in each harbor located on the South East China Sea were gained, through analyzing the storm surge of some harbors on it between Lianyungang and Shantou. The storm surge on the sea is strong. The terrible calamity by storm surge is very easily formed. The arisen time of some maximum storm surge is before tropical cyclone landing, it of some is after, and most of them is between 0 to 6 hours at fore-and-aft tropical cyclone landing. The type of storm surge and the features of each part in the sea areas are very different. Tropical cyclone damages ships and docks reducing battle effectiveness without combat. This paper provides reference for controlling flood and preventing disaster in the summer and fall on the sea areas.

关 键 词：东南沿海 台风增水 最大增水出现时间 增水曲线类型 风暴潮 热带气旋 

分 类 号：P731.23[天文地球—海洋科学] P732