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本研究于1985—1988年在黄东海和热带西太平洋进行了七个航次的大规模海洋环流和海气相互作用考察,取得了700多站次的CTD及其他水文气象高质量的科学资料。写出论文报告30余篇,其中13篇在国际学术会议上发表,19篇在一级刊物上发表。通过研究提出了陆架锋生上升流概念和黄海夏季热生环流新模式。研究结果指出:夏季黄海冷水团下层为单一反时针环流;上层为两个反向环流(两者之间有冷锋和上升流产生);冷水团中心上升流不穿过跃层。从而改变了黄海冷水团中心自上而下为上升流的单反时针环流的传统观点。并得到有关实测资料的证实。
In this study, we conducted a large-scale ocean circulation and air-sea interaction investigation in seven voyages in the Yellow Sea and the tropical West Pacific from 1985 to 1988 and obtained more than 700 stations of CTD and other high-quality hydrological and meteorological data. More than 30 papers were written, of which 13 were published in international academic conferences and 19 were published in first-level publications. Through the research, the concept of upwelling of shelf front and the new model of summer heat circulation in the Yellow Sea are proposed. The results show that: the lower reaches of the Yellow Sea cold pool in summer is a single anticlockwise circulation; the upper two reverse circulation (cold front and upflow between the two); Thus changing the traditional viewpoint that the center of the Yellow Sea chilled water flows from the top to the bottom. And obtained the confirmation of the measured data.