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气象:1999,25(12):24-27
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秋季层状云中高值过冷水区的微物理特征
(山东省气象科学研究所,济南 250031)
The Microphysical Characteristics of High Supercooled Water Area in Stratiform Cloud of Autumn
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中文摘要: 利用11架次的机载“PMS”资料,分析了山东秋季层状云中高值(大于0.1g·m-3)过冷水区的微物理特征:最大过冷水含量为0.361g·m-3,84.0%的过冷水含量在0.1~0.2g·m-3间,过冷水连续出现的宽度86.1%小于3.0km。雪晶形状以霰粒和小雪粒为主。2阶Г函数可以很好地拟合云滴尺度谱,质量谱适合用对数正态函数拟合。
Abstract:The microphysical characteristics in high supercooled water area (higher than 0.1g.m-3) in autumn's strait form cloud over Shandong were analyzed by means of the datafrom measurements with the particle measuring system (PMS) during 11 flights. The maxi. mum water content is 0.369.m-3, 84.0% of supercooled water contents is between 0.1 and0.2g.m-3, 86.1% of continual distribution width of supercooled water is less than 3km.The shapes of snow crystals mainly is graupel and smaller snow crystals. The cloud dropletscale spectrum can be fitted best by two-order Гfunction, and content spectrum can be fittedby log-normal function.
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基金项目:“九五”国家科技攻关项目96-02005,省局“九五”科技重点项目“山东飞机人工增雨条件和催化部位的实时决策系统”课题
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引用文本:
王俊,张连云,陈金敏,王庆,龚佃利,1999.秋季层状云中高值过冷水区的微物理特征[J].气象,25(12):24-27.
,1999.The Microphysical Characteristics of High Supercooled Water Area in Stratiform Cloud of Autumn[J].Meteor Mon,25(12):24-27.