摘要
本文讨论了１９８７年５～６月东海海域溶解氧垂直分布及其氧最大值分布特征。结果表明，春末在东海北部、中部的中层存在明显的溶解氧垂直分布最大值。氧最大值与冷水同存。
In this paper, the vertical distribution of dissolved oxygen and the maximum value in the East China Sea from May to June in 1987 are discussed. The results of study show that the existence of oxygen maximum value at the intermediate layers in the northern and middle areas of the East China Sea was obvious. It is found that the maximum always coexisted with cold water. The relation between the oxygen maximum and its vertical structure and the intrusion of cold water and warm water, and the thermocline are analyzed.
出处
《东海海洋》
1997年第1期1-10,共10页
Donghai Marine Science
关键词
东海
海域
最大值
溶解氧
垂直分布
温跃层
the sea area of the East China Sea, the late spring, the maximum value of dissolved oxygen, cold water and warm water, the thermocline
