台湾暖流与黄海沿岸流 taiwan warm current and huanghai sea coastal current
中层冷水是存在于密跃层之中，高密度（台湾暖流）水的浮力效应使其叠置于它的上方；
It is pointed out that ICW occurs in the pycnocline and superimposes on the pycnocline due to the buoyancy effect of Taiwan Warm Current water with high density.
在计算区域的南部西侧还有一支流，即台湾暖流内侧分支，作气旋式弯曲后，转为东北方向流。
In the west side of the southern part of the computed region, there is other current, which is mainly inshore branch of the Taiwan Warm Current, and it flows cyclonically and turns to northeast.
应用推荐