本文结果为使用双极化雷达研究云降水机制提供了方法，表明双极化雷达在云降水物理的研究中具有广阔的应用前景。
The studies provide the method for dual-polarization radar application to cloud and precipitation physics studies, and indicate its broad potential application prospect.
模拟结果表明，详细云物理过程的考虑对深入理解武汉这次强降水的形成过程是有意义的。
The model results also indicate that the consideration of detailed cloud physical processes is significant for further understanding the formation of this heavy rainfall event.
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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