The frontalcloud 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。
2
The results showed that 51 per cent of storm rainfall was formed by prefrontal convective storm cell, convective cloud in the front of frontalcloud produced 35 per cent of rainfall.