东中国海陆架环流的单层模式
A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA
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摘要: 对于东中国海的环流概况(参看图1),总的来说东中国海的海流是由来自黑潮及其分支、(台湾暖流、黄海暖流)和中国沿岸流两个系统所组成的.关于东中国海海流的研究,国内外已有不少学者做了工作.Abstract: The aim of this paper is to study the paths by which the outflow of the Changjiang River travels through the East China Sea.A verically integrated model including the baroclinic effect is proposed and actual relief is used.The area considered covers from 28°N to 37°30'N, and is bounded by the China's coast on the west and by the Korea's coast or the 127°E on the east.Inputs along the boundary include.
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管秉贤,海洋与湖沼,1(1957),1,95-115. 管秉贤.海洋与湖沼,4(1962),3-4,121-141. 毛汉礼、甘子钧、兰淑芳,海洋与湖沼,5(1963),3,183-206. 近藤正人、玉井一寿,海洋科学,7(通卷63号)(1975),1.27-33 井上尚文,海洋科学,7(通卷63号)(1975),1,12-18. 奚盘根.张淑珍、冯壬筰,山东海洋学院学报,10(1980),3,13-25. -
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