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东南沿海台风风暴潮特点及其变化规律 被引量:11

FEATURE AND VARIED RULE OF TYPHOON STORM SURGE ALONG THE COAST OF SOUTH EAST CIIINA SEA
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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.
出处 《海洋预报》 北大核心 2002年第1期81-88,共8页 Marine Forecasts
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 South East China Sea tropical cyclone surges (TCS) arisen time of Max. TCS curve type of TCS
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参考文献4

  • 1叶锦照(译).风暴增水分析计算[M].广东高等教育出版社,1989..
  • 2国家海洋局.台风浪与增水年鉴[M].海洋出版社,1968-1982..
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  • 4中央气象局.台风年鉴[M].气象出版社,1949-1990..

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