For these reasons, a half-close and clockwise or counter-clockwise flow circulation is formed at the north of the bay during tide falling or rising.

因此，涨潮时北半部形成一个半封闭式的逆时针向环流，落潮时则形成半封闭式的顺时针向环流。

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For these reasons, a half-close and clockwise or counter-clockwise flow circulation is formed at the north of the bay during tide falling or rising.

因此，涨潮时北半部形成一个半封闭式的逆时针向环流，落潮时则形成半封闭式的顺时针向环流。

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