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大气科学  2006 

Characteristics of Rain from Stratiform Versus Convective Cloud Based on the Surface Raindrop Data
基于地面雨滴谱资料分析层状云和对流云降水的特征

Keywords: disdrometer,raindrop size distribution,stratiform cloud,convective cloud
声雨滴谱仪
,雨滴谱,层状云,对流云

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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.

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