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.
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；
Sea winds that blow inland from the west are warmed by a current of warm water that flows through the Pacific Ocean.
从太平洋来的温暖的洋流使得从西吹过内陆的海风变得温暖。
It is a current of warm water.
这是一股暖水流。
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