云和降水粒子的非球形性质是引起雷达散射信号产生退偏振的主要因素。
The major factor which produces the depolarization of radar scattering signals is the non-spherical properties of hydrometeors.
同时给出的ZH与ZDR和KDP关系公式也基本不受雨滴谱变化的影响，它可以用于降水粒子相态的识别。
The relationship between ZH and ZDR, and KDP is not sensitive to the variations of DSD, which could be used in distinguishing the solid precipitation from rain.
观测事实表明，对流云中分布着许多不同大小的云泡，本文根据这一事实讨论有云泡结构的对流云中降水粒子形成的问题。
The formation of precipitation in convective cloud with cell structure is inve-stegated, based on the fact that a cloud consists of a great deal of cells in different phases.
应用推荐