摘要
在我国,关于黄海、东海温、盐度逆转结构的分析研究,主要是在80年代以后开始的。翁学传等(1984)、曹欣中等(1982)和丁宗信(1983)对东海某一特定海域的温、盐度逆转结构进行过分析,但是对整个黄海、东海海区来说。
Based on temperature and salinity data gathered from 1963 through 1986 in the Yellow Sea and the East China Sea in summer, the distributional characteristics of the inverse structure of the temperature and salinity and its formative causes are analysed in this paper. Some results show that (1) the inverse structure in summer can be found in three regions, the area of the Zhejiang Coast upwelling, the area of the cold eddy in the northern part of the East China Sea and the area of cold water mass in the southern Yellow Sea, (2) the inverse structure in above three areas can be separately caused by the wind, the vertical circulation in the area of the cold eddy,and the northward extension of the Huanghai warm current water which is warmer and more saline in bottom.
出处
《海洋科学集刊》
CAS
1994年第1期11-21,共11页
Studia Marina Sinica
基金
国家自然科学基金
编号 49176254
