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