黄海沿岸流

黄海沿岸流是控制研究海区表层沉积物沉积作用的主要水动力因素，沿岸流主轴线上沉积物较粗，向其两侧和沿流向沉积物变细。

The Yellow Sea Coastal Current ( YSCC ) is the major dynamical factor that dominates the transportation and sedimentation of surface sediments .

这些都表明晚全新世晚期低温、低盐、高营养的黄海沿岸流加强。3.6-1.95kaB.P.碳氧同位素的高值表明这一阶段，研究区主要受高温、高盐、低营养的黄海暖流的影响。

All of this shows that the study area was strong influenced by Yellow sea coast current which has a characteristic of low temperature , low salinity and high nutrient during the late of late Holocene .

对马暖流为在黑潮主干西侧沿100～200m等深线流动的一支海流与黄海大陆沿岸流的混合。

The Tsushima is a mixture of the current flowing along the 100-200m isobath on the west side of the Kuroshio and the coastal current in the Yellow Sea .

冬季，黄海东部朝鲜沿岸流南下过程中，有三分支脱离其主体向黄海内部流动并形成三个涡旋。

Three branches separating from Kuroshio flow toward the interior of the Yellow Sea , and formate three eddies respectively .

同时，模式很好地模拟了该海域的黑潮、台湾暖流、对马暖流、黄海暖流以及沿岸流等主要环流。

The model has simulated Kuroshio , Taiwan Warm Current , Tsushima Current , the Yellow Sea Warm Current , and Coast Current .