龙口港湾大振幅假潮的成因分析
A cause giving rise to large amplitude seiches in the Longkou Bay
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摘要: 龙口湾位于山东半岛北部,莱州湾东北隅,为莱州湾的一个附属海湾.海湾湾口朝向西南,湾廓近似半圆形,属半封闭海湾.龙口验潮站位于湾顶(图1),水深7m.
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陈则实,李坤平.山东半岛沿岸的大振幅假潮[J].黄渤海海洋,1999,17(4):1~12. GOMIS D,MONSERRAT S,TINTORE J.Pressure-forced seiches of large amplitude in inlets of the Balearic Islands [J].J G R,1998,98(C8):14 437~14 495. GARCIES M,GOMIS D,MONSERRAT S.Pressure-forced Seiches of large amplitude in inlets of the Balearic Islands,2.Observational study [J].J G R,1996,101(C3):6 453~6 467. TOSHIYUKI H,KINGIRO K.Origin of the Abiki phonomenon(a kind of seiche) in Nagasaki Bay [J].J Oceanogir Soc Japan,1982,38:172~182. 王兴铸,李坤平,余宙文.龙口港内港湾振动的概要特征[J].海洋湖沼通报,1986,(2):1~5. WILSON B W.The Encyclopedia of Oceanography [Z].Encyclopedia of Earth Sciences Series,Vol.1,Donden,Hutchinson and Ross.Inc.Stroudsburg Pennsylvania,1966.804~817. 郭洪寿,王喜年,赵俊昌.黄渤海温带风暴潮的初步分析[J].风暴潮,1981,(2):6~15. 杨华庭等主编.中国海洋灾害四十年资料汇编(1949~1990)[Z].北京:海洋出版社,1993.22~30.
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