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首页> 外文期刊>SOLA: Scientific Online Letters on the Atmosphere >Microphysical Structures of Early-Winter Snow Clouds during a Cold Air Outbreak of December 23-25, 2010
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Microphysical Structures of Early-Winter Snow Clouds during a Cold Air Outbreak of December 23-25, 2010

机译：2010年12月23日至25日的冷空气爆发期间初冬雪云的微观物理结构

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References(20) Cited-By(2) Supplementary materials(1) A series of videosondes that were continuously launched revealed the microphysical structures of snow clouds during the entire period of an intense cold air outbreak that occurred during December 23-25, 2010. The evolution of the microphysical features of graupel and snowflakes associated with the cold air outbreak were examined. It was found that the precipitation particle distributions in the snow clouds varied as the development of the cold air outbreak progressed. Graupel was the predominant precipitation particle throughout the cold air outbreak, while the number of snowflakes was increasing in the latter half of the period. When the lightning activity was relatively weak, high concentrations of graupel were located at lower level warmer than ?10°C. It is suggested that lightning activity is associated with the vertical distribution of graupel.
机译：参考文献（20）被引用的辅助材料（2）补充材料（1）一系列连续发射的探空仪揭示了在2010年12月23日至25日发生的强烈冷空气暴发的整个期间，雪云的微物理结构。研究了与冷空气暴发有关的gra和雪花的微物理特征的演变。研究发现，随着冷空气爆发的发展，雪云中的降水颗粒分布也发生了变化。在整个冷空气爆发期间，Graupel是主要的降水颗粒，而在此期间的后半段，雪花的数量在增加。当雷电活动相对较弱时，高浓度的up在低于10°C时处于较低水平。建议雷电活动与gra的垂直分布有关。

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