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主要根据1992年8月中国科学院南海海洋研究所和香港理工大学合作进行的“南海环流试验”的调查资料,并引用中国科学院南海海洋研究所1982年7月、1985年8月在南海东北部的调查资料、黑潮合作调查(CSK)的资料,通过温、盐度分布特征的分析,并结合动力计算结果,指出夏季在南海东沙群岛北侧存在着一偏西向海流,它的流动路径与文献[5-7]中所说的南海黑潮分支的流动路径显著不同。对夏季南海海流的三维数值模拟也得到了相似的结果。
According to the survey data of the South China Sea Circulation Experiment conducted in cooperation with the South China Sea Institute of Oceanology, Chinese Academy of Sciences in August 1992 and the Hong Kong Polytechnic University, and quoted the South China Sea Institute of Oceanology, Chinese Academy of Sciences in July 1982 and August 1985 in the northeastern part of the South China Sea According to the survey data and the data from the Kuroshio Cooperative Investigation (CSK), based on the analysis of the distribution of temperature and salinity, combined with the dynamic calculation results, it is pointed out that there is a westward current in the north of the Dongsha Islands of the South China Sea in summer. The flow path of the Kuroshio in the South China Sea is remarkably different in [5-7]. Similar results were obtained for the three-dimensional numerical simulation of the summer South China Sea current.