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气象:2012,38(9):1129-1134
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2003年春季陕西省层状云降水的雨滴谱特征
(1.陕西省人工影响天气办公室,西安 710015;2.中国气象科学研究院,北京 100081)
Characteristics in Size Distribution of Raindrops of Stratiform Precipitation in Spring 2003 of Shaanxi Province
(1.Weather Modification Office of Shaanxi Province, Xi’an 710015;2.Chinese Academy of Meteorological Sciences, Beijing 100081)
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投稿时间:2011-05-13    修订日期:2012-03-06
中文摘要: 文章给出了陕西省春季(2003年)层状云降水雨滴谱部分特征,这些特征与降水天气系统密切相关。降水产生于混合云,各层系统配置适当,有较厚冷层云和相接的暖层云,雨滴数浓度大可达103 m-3,雨滴谱较宽可达0.32 cm。反之数浓度较小(102 m-3),谱较窄(0.22 cm)。其中直径0.1 cm以下雨滴谱约占总浓度的80%以上,而对雨强的贡献小于20%。0.1~0.2 cm雨滴是雨强的主要分量,它平均占48%~77%。雨滴谱多数呈非单调下降分布,三参数分布n(Di)=n0Dαe-λD明显优于指数分布n(Di)=n0e-λD。
Abstract:Some features of raindrop spectrum in stratiform clouds in spring 2003 of Shaanxi were observed and analyzed in this paper, which are closely associated with precipitating weather systems. The precipitating mixed clouds with deeper cold and warm cloud layers have an appropriate level configuration, and their raindrop number concentrations are bigger up to 103 m-3 and the spectra of raindrops are wider up to 0.32 cm. Conversely, the stable clouds have a smaller number concentration (102 m-3) and a narrower spectrum width (0.22 cm). The raindrops under 0.1 cm in diameter accounted for more than 80% of the total concentration, while the contribution to rainfall intensity is less than 20%. Actually, the 0.1-0.2 cm across raindrop is a major component of rainfall intensity, which accounted for an average 48%-77%. The majority of raindrops had a non monotonic decreased spectral distribution, and the three parameter fitting formula n(Di)=n0Dαe-λD is better than the exponential distribution n(Di)=n0e-λD.
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基金项目:国家科技部“西部开发科技行动”重大攻关项目(2001BA901A41)课题资助
引用文本:
罗俊颉,贺文彬,李金辉,严采蘩,陈万奎,2012.2003年春季陕西省层状云降水的雨滴谱特征[J].气象,38(9):1129-1134.
LUO Junjie,HE Wenbin,LI Jinhui,YAN Caifan,CHEN Wankui,2012.Characteristics in Size Distribution of Raindrops of Stratiform Precipitation in Spring 2003 of Shaanxi Province[J].Meteor Mon,38(9):1129-1134.