我们曾基于底摩应力涡度、行星涡度和风应力涡度的平衡方程,在黑潮(边界力(奚盘根等,1980,冯士搾等,198l。))可变海底地形的作用下,研究了东中国海环流的可能成因(刘凤树等,1984)。指出,东中国海环流的形成主要是黑潮作用的结果,风的效应仅起调 Based on the equilibrium equations of bottommoidal stress vorticity, planetary vorticity and wind stress vorticity, we studied the effects of the Kuroshio (boundary force (Xi Pangen et al., 1980, Feng Shijie et al., 198l.)) Variable submarine topography Possible Causes of Circulation in China Sea (Liu Fengshu et al., 1984). Pointed out that the formation of the circulation of the East China Sea is mainly the result of the Kuroshio effect and the effect of the wind is only raised