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密集的正地闪也与强回波区相对应，而稀疏的正地闪则多发生在系统后部的稳定性降水或云砧部位。
Moreover, the dense positive CG flashes can also be observed in the strong echo region, while sparse ones are in the weak and stable echo region or cloud anvil in the rear MCS.
在季节尺度，对流云和层状云降水的比与两者的面积比成比例关系。
On a seasonal scale, the results indicate that the rainfall ratio of stratiform rain to deep convective rain is proportional to their rainfall pixel ratio.
由于水云与冰云的垂直配置，降水对水云与冰云辐射过程的响应是不同的。
The radiative effects of water- and ice-clouds on rainfall are different due to their vertical profiles.
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