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Structural Characteristics of the Clouds and Precipitation in a Low Vortex Rainstorm Process

机译:低涡暴雨过程中云和降水的结构特征

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Based on the satellite data and conventional observed data, the Structural Characteristic of the Clouds and Precipitation in a Low Vortex Rainstorm Process during June 25-26 of 2005 are analyzed. Results show that the rainstorm is associated with the meso-scale convective clouds (MCSs), the structures of which experience the evolvement such as generating, strengthening, coalescing, weakening and so on, and the lowest Black Body Temperature (TBB) ofwhich can be -90degC. The spatial and temporal distribution is inhomogeneous in the cumulous and stratiform mixed clouds. In the upper area of the convective clouds there is a high value area of ice crystal, below which there is more cloud water than surrounding, and the warm rain feature is remarkable. The researches on the forming conditions of rainstorm suggest that the southwest (SW) vortex suppliessuch beneficial conditions for it as vapor, dynamic convection and instability.
机译:基于卫星数据和常规观察数据,分析了2005年6月25日至26日在2005年6月25日至26日的低涡流暴雨过程中云层和降水的结构特征。结果表明,暴雨与中学规模的对流云(MCS)有关,该结构的经验经历的演变,如发电,加强,聚结,削弱等,以及最低的黑体温度(TBB) -90degc。空间和时间分布在累积和层状混合云中不均匀。在对流云的上部区域,有一个高值的冰晶区域,下面有比周围更多的云水,并且温暖的雨量是显着的。对暴雨成形条件的研究表明,西南(SW)涡流为其作为蒸气,动态对流和不稳定性的益处。

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