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基于地面雨滴谱资料分析层状云和对流云降水的特征
引用本文:刘红燕,雷恒池.基于地面雨滴谱资料分析层状云和对流云降水的特征[J].大气科学,2006,30(4):693-702.
作者姓名:刘红燕  雷恒池
作者单位:1.中国科学院大气物理研究所中层大气遥感与探测开放实验室,北京,100029
基金项目:科技部科研项目;中国科学院资助项目
摘    要:根据由声雨滴谱仪器测量得到的雨滴谱资料,结合降水云的结构来将降水云系划分成为对流云降水云系和层状云降水云系.分析这两种降水云系中的稳定雨滴谱特征,包括雨滴谱的各种特征直径(平均直径Dm、众数直径Dd、平均体积直径Dv、优势直径Dp、中数直径Dna和中数体积直径Dn)、峰值结构和Z-R关系等.通过对这些量的分析,进一步分析划分降水云系的判据.

关 键 词:声雨滴谱仪    雨滴谱    层状云    对流云
文章编号:1006-9895(2006)04-0693-10
收稿时间:2005-05-08
修稿时间:2005-05-082005-09-05

Characteristics of Rain from Stratiform Versus Convective Cloud Based on the Surface Raindrop Data
LIU Hong-Yan and LEI Heng-Chi.Characteristics of Rain from Stratiform Versus Convective Cloud Based on the Surface Raindrop Data[J].Chinese Journal of Atmospheric Sciences,2006,30(4):693-702.
Authors:LIU Hong-Yan and LEI Heng-Chi
Affiliation:1 Laboratory for Middle Atmosphere and Global Environment Observation, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029 ;2 Laboratory of Cloud - Precipitation Physics and Severe Storms, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing 100029
Abstract:It is very meaningful to separate the precipitation cloud system into convective cloud and stratiform cloud.The separation is important to improve the remote sensing of precipitation and compute the heat momentum,and so on.The raindrop size distribution and the structure of precipitation cloud are used to separate the precipitation cloud system into convective cloud and stratiform cloud.In Beijing,the time of convective precipitation is short.Some convective precipitation lasts just half an hour.Moreover,during the precipitation,there often exists lightning and thunder.The time of stratiform precipitation,which lasts at least 5 hours,is longer than that of convective precipitation.The bottom of stratiform cloud is low and has mean structure.First of all,the equilibrium raindrop size distributions are analyzed.The equilibrium raindrop size distributions are continuous and have the similar characteristics in the width of the spectra and maximum of N(D),and so on.Six kinds of diameters are calculated,including the mean diameter D_(m),the mode diameter D_(d),the mean volume diameter D_(v),the predominant diameter D_(p),the median volume diameter D_(n) and the median diameter D_(nd).It is found that for convective cloud D_(v)>1.20 mm,and D_(n) >1.5 mm.The peak of raindrop size distribution is analyzed.There is no single peak of raindrop size distribution in the convective precipitation,however,there exists in stratiform precipitation.The raindrop size distributions are separated into 3 kinds,such as single-peak raindrop size distribution,double-peak raindrop size distribution and three-peak raindrop size distribution.The diameters corresponding to the peaks are analyzed.The rain-rate R and the radar reflectivity factor Z are calculated using the equilibrium raindrop size distribution,and then the relationship between R and Z are calculated.Compared with the stratiform cloud precipitation,the factor of the relationship is high for convective cloud precipitation.The factor is lager than 200 for convective cloud precipitation,and the factor is smaller than 200 for stratiform cloud precipitation.All the informations can be used to separate precipitation cloud into convective cloud and stratiform cloud.But the precipitation is complex,so it should be careful to use one of the informations.
Keywords:disdrometer  raindrop size distribution  stratiform cloud  convective cloud
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