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根据1992年5月在南黄海取得的CTD资料和两个断面（34°N，36°N）的温、盐度和溶解氧资料，利用“对应分析法”研究该海域的水团配置和特性，并对其中的某些问题进行探讨。结果表明：春季，南黄海海域存在8个水团，即黄海水、南黄海冷水团、青岛冷水团、黄海暖流水以及长江冲淡水、苏北沿岸水、成山角冷水和朝鲜西岸沿岸水；南黄海冷水团是由黄海本地冷水和黄海暖流变性水组成，其内部的温、盐性质并不十分均匀；青岛冷水团来源于黄海沿岸水（渤南沿岸水），具有独特的温、盐结构和长消过程，是一个独立的水团而不是南黄海冷水团的组成部分。
Based on the CTD data acquired in the South Yellow Sea in May 1992 and the temperature, salinity and dissolved oxygen data of two sections (34 ° N, 36 ° N), the “corresponding analysis method” was used to study the water mass configuration and characteristics , And discuss some of them. The results show that in the spring, there are 8 water masses in the South Yellow Sea, namely Yellow Sea Water, South Yellow Sea cold water mass, Qingdao Cold Water Mass, Yellow Sea warm water, Yangtze River red water, northern Jiangsu Sea water, Chengshan River cold water and North Korea coast water; The Yellow Sea cold water mass is composed of the Yellow Sea local cold water and the Yellow Sea warm current denatured water, and the internal temperature and salinity properties are not very uniform. The cold water mass derived from the Yellow Sea coast water (Bonan coastal water) has unique temperature and salt structure Long disappear process, is an independent water regiment rather than a component of the South Yellow Sea cold water regiment.