It is pointed out that ICW occurs in the pycnocline and superimposes on the pycnocline due to the buoyancy effect of TaiwanWarmCurrent water with high density.
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；
2
In the west side of the southern part of the computed region, there is other current, which is mainly inshore branch of the TaiwanWarmCurrent, and it flows cyclonically and turns to northeast.