Some Striking Features of Circulation in Huanghai Sea and East China Sea
Some Striking Features of Circulation in Huanghai Sea and East China Sea
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DOI：
10.1007/978-94-011-0862-1_4
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发表时间：
1994
影响因子：
4.3
通讯作者：
Hu Dun-xin
中科院分区：
文献类型：
--
作者：
Hu Dun-xin
只有当垂直运动的速度达到一个大得多的值时，例如10-5 cm/s到10-cm/s的量级时，才认为垂直运动是上升运动。黄海和东海有几个上升流区（图1）（Guan，1963; Hu et al.，1980年，1984年）。本文仅讨论浙江沿海的上升流，这对渔业和了解其物理过程都有重要意义。
A vertical motion is considered as upweIIinfo only where or when its velocity reaches a much larger value, say, 10-5 cm/s to 10-cm/s in order of magnitude. There are several areas of upwelling in the Yellow Sea and East China Sea (Fig. 1)(Guan, 1963; Hu et al., 1980, 1984). In this section, only the coastal upwelling off the Zhejiang Province will be dIscussed, which is significant for both fishery and the understanding of its physical process.