论述有关发生在高纬度海洋上的极地低压研究的最新进展。

This paper deals with the recent advances on the study of polar lows occurred over the high latitude oceans.

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同一时期，海洋散热较慢，温度相对地较高，空气密度变化较小，遂形成相对的低压区。

The same period, the ocean thermal slow, relatively high temperature, air density changes smaller solipsism relative area of low pressure.

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在印度洋上空，这潮湿的海洋空气被扯进高压区，并向南移向低压区。

All this wet air is pulled in by a high pressure area over the Indian Ocean and a low pressure area to the south.

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在印度洋上空，这潮湿的海洋空气被扯进高压区，并向南移向低压区。

All this wet air is pulled in by a high pressure area over the Indian Ocean and a low pressure area to the south.

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