云微物理场的模拟显示没有雪出现，这可能是华南降水云微物理的特点；
There were no snow in the simulated results, and it was due possibly to the particular cloud microphysics field of South China.
层状云由于在水平上较为均匀， 可以用一维模式来模拟其云微物理过程。
The stratiform cloud can be simulated with a one-dimensional model, duo to its uniform horizontal distribution of physical characters.
降水过程的云微物理结构的观测和催化效应的分析在人工增雨中占有重要的地位。
The observation of cloud microphysical structure and the analysis of seeding physical effect play an important role in artificial precipitation-enhancement.
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