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东中国海陆架环流的单层模式
引用本文:袁耀初,苏纪兰,赵金三.东中国海陆架环流的单层模式[J].海洋学报,1982,4(1):1-11.
作者姓名:袁耀初  苏纪兰  赵金三
作者单位:国家海洋局第二海洋研究所
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.

收稿时间:3/2/1981 12:00:00 AM

A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA
Yuan Yaochu,Su Jilan and Zhao Jingsan.A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA[J].Acta Oceanologica Sinica (in Chinese),1982,4(1):1-11.
Authors:Yuan Yaochu  Su Jilan and Zhao Jingsan
Institution:Second Institute of Oceanography National Bureau of Oceanography Hangzhou
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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