From south to north, the Yellow Sea warm current separates the circulation of Yellow Sea into two parts.
黄海暖流从南向北将黄海环流分成东西两部分。
It is discovered, that sedimentary system have been controled by the Yellow Sea warm current and its derivative (cold eddy system).
经分析发现，这个沉积体系，完全受控于黄海暖流、冷涡及其相关的环流体系。
Numerical experiments based on POM are carried out to study the forming mechanism of this thermal structure and its relation to the Yellow Sea Warm Current (YSWC).
数值实验结果表明：西暖舌是由黄海暖流形成的，而黄海暖流由于冬季季风海流的补偿作用而得到加强。
Numerical experiments based on POM are carried out to study the forming mechanism of this thermal structure and its relation to the Yellow Sea Warm Current (YSWC).
数值实验结果表明：西暖舌是由黄海暖流形成的，而黄海暖流由于冬季季风海流的补偿作用而得到加强。
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