Kuroshio Intrusion and Taiwan Warm Current
Kuroshio Intrusion and Taiwan Warm Current
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DOI：
10.1007/978-94-011-0862-1_7
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发表时间：
1994
影响因子：
10.5
通讯作者：
Su Jilan;Pan Yuqiu;Liang Xiang-san
中科院分区：
文献类型：
--
作者：
Su Jilan;Pan Yuqiu;Liang Xiang-san
东海的大部分海域是广阔的浅海陆表海的一部分，其北部包括半封闭的黄海（图1）。西南经台湾海峡与南海相连，东北经朝鲜海峡与日本海相连。琉球群岛的东部和南部是北太平洋。黑潮在台湾以东进入东海。它沿着大陆架边缘流动，直到大约29 - 30 'N，在那里它离开大陆架，通过托卡拉海峡重新进入太平洋。台湾东北部的所有观测都有黑潮入侵陆架的证据（苏和潘，1990）。
A large area of the East China Sea (ECS) is a part of a broad shallow epicontinental sea which includes the semi-enclosed Huanghai (Yellow) Sea to the north (Fig. 1). It is connected with the South China Sea at the southwest through the Taiwan Strait and to the Japan Sea at the northeast through the Korea Strait. East and south of the Ryukyu Archipelago is the North Pacific Ocean. Kuroshio enters the ECS east of Taiwan. It flows along the shelf edge until around 29 30'N where it leaves the shelf and re-enters the Pacific Ocean through the Tokara Strait. All observations northeast of Taiwan have always yielded evidence of the intrusion of Kuroshio water onto the shelf (Su and Pan, 1990).