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本文主要根据1985年9月台湾暖流专题调查所取得的海流和温、盐度资料,对夏末、秋初台湾海峡水进入东海后的运移路径和混合情况,进行了比较详细的分析研究。得出,台湾海峡水进入东海后仍以NNE方向流动,约在福建北部外海(27°N以北,121°45′E以东)开始楔入来自台湾东北的黑潮表层水之中,并与其发生混合形成台湾暖流表层水。这一结果进一步证明了作者以前提出的关于台湾暖流来源的看法是符合客观实际的。
In this paper, based on the ocean current and temperature and salinity data obtained from the survey of Taiwan’s warm current in September 1985, a detailed analysis is made of the migration path and mixing of the Taiwan Strait water entering the East China Sea in late summer and early autumn. Concluded that the Taiwan Strait still flows in the NNE direction after entering the East China Sea and wedges into surface Kuroshio water from northeastern Taiwan about the northern coast of Fujian (north of 27 ° N and east of 121 ° 45’E) With its mixing to form the surface warm water in Taiwan. This result further proves that the author’s previous opinion on the source of the warm current in Taiwan is in line with the objective reality.