总环流在表层基本上为朝西北的流动，在底层同样出现向东南的回流，主要是由风应力驱动的。
The combined surface currents flow northwestward flow, while the bottom compensation currents flow southeastward. The combined circulation is mainly driven by the wind.
总环流在表层基本上为朝西北的流动，在底层同样出现向东南的回流，主要是由风应力驱动的。
The combined surface currents flow northwestward flow, while the bottom compensation currents flow southeastward. The combined circulation is mainly driven by the wind.
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