摘要
多年来，很多国内外学者对东中国海环流的机理进行了研究。近几年，奚盘根等(1980)和冯士筰等(1981)基于f-坐标系的风涡度一热盐梯度全流方程分别数值地模拟了冬、夏季东中国海环流。他们指出，控制东中国海环流主要因子是边界力(黑潮)、热盐力和底形分布。袁耀初等(1982)也数值地模拟了东中国海环流结构，
In this paper the winter and summer circulations in the East China Sea are described by using the two-dimensional equation of steady-state with a linear bottom friction. Analysis shows that the boundary forces (Kuroshio System) plays a determinant role and the wind stress onlyacts as an adjustment factor in generation of the circulation.
