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关于南海的环流系统已进行了一些研究。早期的研究成果主要是根据船舶漂移和风场资料描绘了表层海流图。六十年代初期,wyrtki用动力学观点对南海的水平环流进行了探讨。七十年代以来,williason,Kwan Ming Chan,watts,Uda和Nakao等进一步讨论了南海北部的水文和海流状况。但是,这些研究都有一个大致相同的结论,即表层流或环流大体上与盛行季风的方向一致。
Some research has been conducted on the circulation system in the South China Sea. Early results of the study were mainly based on ship drift and wind field data depicting the surface current map. In the early 1960s, wyrtki discussed the horizontal circulation in the South China Sea from a kinetic point of view. Since the 1970s, Williason, Kwan Ming Chan, Watts, Uda and Nakao discussed further the hydrological and current conditions in the northern South China Sea. However, all of these studies have the same general conclusion that the surface or circulation generally corresponds to the prevailing monsoon.