The frontal cloud is mainly stratocumulus, with a limited depth as a result of the subsidence inversions in both air masses.

锋面云系主要是层积云，由于在冷暖空气团中下沉逆温的作用，云系的厚度受到了限制。

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The results showed that 51 per cent of storm rainfall was formed by prefrontal convective storm cell, convective cloud in the front of frontal cloud produced 35 per cent of rainfall.

分析指出，暴雨51%的雨量由锋前对流风暴单体形成，有35%的雨量为锋面云系前部的对流云产生。

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