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气象:2014,40(1):59-65
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2009年初冬山东一次暴雪过程粒子谱特征分析
(山东省人民政府人工影响天气办公室,济南 250031)
Characteristics of Particle Spectrum During the Snowstorm Process in Early Winter 2009 in Shandong Province
(Shandong Weather Modification Office, Jinan 250031)
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投稿时间:2012-10-08    修订日期:2013-06-24
中文摘要: 为了研究降雪过程中粒子微物理特征,利用架设在济南南部山区的一台THIES激光降水粒子谱仪获取的2009年11月11—12日强降雪过程中降水粒子谱资料,对降雪粒子微物理参量演变特征、粒子谱及速度谱分布特征进行了分析。结果表明,(1)此次降雪天气过程中降水强度与数浓度、最大直径和雷达反射率因子间均具有一定的正相关性;降水强度与最大直径的关系极为密切,粒子的大小直接决定降水强度的大小。(2)降雪过程中谱型分布以单峰型和指数型为主,各粒径档内数浓度分布存在不均匀性,但数浓度峰值直径主要集中在0.5 mm处。(3)粒子速度谱均以单峰结构分布,下落末速基本位于0.375~2 m·s-1之间,随直径的增大几乎没有变化。
Abstract:To better study microphysical characteristics during snowfall process, drop size spectra were collected with an optical disdrometer during the snowstorm event in 11-12 November 2009 in the southern mountainous area of Jinan. The characteristics of the microphysical parameters, the drop size distribution and speed spectral distribution are investigated. It is found that: (1) during the snowstorm, precipitation intensity and number concentration, maximum diameter, and the radar reflectivity factor have positive linear correlations; the precipitation intensity and the maximum diameter has a close relationship; precipitation intensity is decided by the maximum diameter. (2) In the snow process, the spectrum type distributions are of unimodal and index distributions, and the peak value of number concentration is focuses around 0.5 mm. The concentration distribution of each particle size file is inhomogeneous. (3) The velocity spectra are mainly single peak distributions, and the terminal velocity essentially lies in the range of 0.375-2 m·s-1, which almost has no change with the increase of diameter.
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基金项目:山东省气象局课题(2013sdqx19、2012sdqxz07和2012sdqx12)共同资助
引用文本:
周黎明,王俊,龚佃利,张洪生,2014.2009年初冬山东一次暴雪过程粒子谱特征分析[J].气象,40(1):59-65.
ZHOU Liming,WANG Jun,GONG Dianli,ZHANG Hongsheng,2014.Characteristics of Particle Spectrum During the Snowstorm Process in Early Winter 2009 in Shandong Province[J].Meteor Mon,40(1):59-65.