A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA

Yuan Yaochu; Su Jilan; Zhao Jingsan

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Yuan Yaochu, Su Jilan, Zhao Jingsan. A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA[J]. Haiyang Xuebao, 1982, 4(1): 1-11.

Citation:

Yuan Yaochu, Su Jilan, Zhao Jingsan. A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA[J]. Haiyang Xuebao, 1982, 4(1): 1-11.

Yuan Yaochu, Su Jilan, Zhao Jingsan. A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA[J]. Haiyang Xuebao, 1982, 4(1): 1-11.

Citation:

Yuan Yaochu, Su Jilan, Zhao Jingsan. A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA[J]. Haiyang Xuebao, 1982, 4(1): 1-11.

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A SINGLE LAYER MODEL OF THE CONTINENTAL SHELF CIRCULATION IN THE EAST CHINA SEA

Second Institute of Oceanography National Bureau of Oceanography Hangzhou

Received Date: 1981-03-02

Abstract

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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