东海陆架波及其对黑潮的影响
-
摘要: 本文将自由陆架波理论用于东海沿岸陆架的实际情况,以分析陆架波与黑潮的联系.结果表明,低频陆架波自北向南运动,其相速度正比于黑潮的流速,黑潮的最大流速位于陆缘处.分析解的形式还表明,陆架海域呈现带状结构的水文特征,由陆架波在陆缘处引起的垂直于岸线的水平运动可能是产生黑潮流轴波状花纹的原因之一.
-
Hamon B.V.The spectrums of mean sea level at Sydney,Coff's Harbour,and Lord Howe Island.J.Geophys.Res.,1962.,67,5147-5155 Hamon B.V.Correction to the spectrums of mean sea level at Sydney,Coff's Harbour,and Lord Howe Island.J.Geophys.Res.,1963,68(15):4635 陈大可,苏纪兰.中国沿海陆架波的初步分析.海洋学报,1967,(1):1-15 Mysak L.A,On the theory of continental shelf waves.J.Marine Res.,1967,25(3):205-226 Robinson A.R.Continental shelf wave and the response of sea level to weather systems.J.Geophys.Res.,1964,69(2):367-368 Caldwell D.R.,D,L.Cutchin and M.S.Longuet-Higgins.Some model experiments on continental shelf waves.J.Marine Res.,1972,30,39-55 Toshiyuki Hirano,Kuroshio Explotation and Utillization Research Summary Report 1977-1982,page 40,(Edited by project leaders committee for Kuroshio research,Issued by Japan Marine Science and Tethnology Center.) 管秉贤.东海黑潮变异研究的若干结果.海洋与湖沼,1979,10(4);297-306 -
计量
- 文章访问数: 721
- HTML全文浏览量: 15
- PDF下载量: 690
- 被引次数: 0
下载:
