...南黄海后由于沉积环境的变化，很少量物质会在渤海沿岸流的影响下向成山头的南面或者东南方向扩散，扩散范围东部以黄海暖流(YSWC)为界，南部则会到达35°N左右[ 36]; 该区域沉积物的沉积环境、 物源和沉积作用一直处于稳定状态[
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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。
It is shown from the analysis of formation mechanism that the pressure gradient force, vertically frictional force and Coriolis force play the leading roles in forming the YSWC.
对黄海暖流形成机理的分析表明，压强梯度力、垂向摩擦力和柯氏力占主要地位。
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