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本文就近几年作者在黄海南部和东海北部进行调查研究(夏季)的主要成果予以阐述,结论为:(1)南黄海底层冷水可进一步划分为三个次级水团;(2)潮混合对黄海冷水团边界和黄海温跃层等有重要影响,它还形成海面的陆架锋;(3)夏季南黄海上层存在着闭合的密度环流,而黄海沿岸流性质上属锋面强流,济州岛西南存在着气旋式海水运动;(4)黄海暖流不再深入黄海冷水团内部,但其内部可能存在着方向相反的一对弱环流;(5)长江口海区存在着可能是因台湾暖流逆坡行进产生的上升流现象。
In this paper, the author summarizes the main findings of the survey conducted in the southern Yellow Sea and the northern part of the East China Sea in the recent years (summer), and concludes that: (1) the cold water in the southern Yellow Sea can be further divided into three secondary water masses; (2) The Yellow Sea cold-water mass boundary and the Yellow Sea thermocline, etc. It also forms a shelf front on the sea surface. (3) There is a closed density circulation in the upper Yellow Sea over the Yellow Sea in summer, (4) the Yellow Sea warm current is no longer deep inside the Yellow Sea cold water mass, but there may exist a pair of weak circulation in the opposite direction. (5) There may be a series of weak circulation due to the reverse current of Taiwan’s warm current The resulting upflow phenomenon.