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DOI10.1016/j.atmosres.2020.104895
Raindrop size distribution and microphysical characteristics of a great rainstorm in 2016 in Beijing, China
Luo L.; Xiao H.; Yang H.; Chen H.; Guo J.; Sun Y.; Feng L.
发表日期2020
ISSN0169-8095
卷号239
英文摘要This paper analyzes the characteristics of rain drop size distributions (DSDs) and vertical profiles of hydrometeors for a severe rainstorm event that occurred in Beijing, northern China, from 19 to 21 July 2016 using in situ measurements from two disdrometers (OTT-Parsivel2 and 2D-Video-Distrometer) and remote sensing data collected by a second-generation Micro Rain Radar (MRR2). This rainstorm was characterized by stratiform precipitation with embedded strong convection on 19 July and widespread, intense mixed convective-stratified rainfall resulting in persistent rainfall between 20 and 21 July. The temporal and spatial variations in rainfall rate R, liquid water content W, reflectivity Z, DSDs and the gamma DSD parameters in different precipitation episodes of this event are derived and compared between two meteorological stations in Beijing. Rainfall throughout the entire event was characterized by large concentrations of small- to medium-sized raindrops (diameters between 2 and 4 mm) and few larger particles (D > 4 mm), resulting in small values of reflectivity Z (<40 dBZ) and liquid water content W (<1.0 g m−3). In addition, the log10Nw-Dm scatter pairs recorded during the convective phase of this rainstorm indicate maritime-like convection. The time evolution of DSDs shows that most single peak DSDs occurred during stratiform rainfall, and bimodal DSDs were observed when the convective rainfall cells passed by and collisional breakups occurred. The gamma DSD model with a single peak in the stratiform phase of the storm and the bimodal DSD in the convective episode of the storm are quantitatively evaluated. In addition, in each precipitation episode, the differences in exponent b and coefficient A of the Z-R relationship between the two stations are smaller for stratiform rainfall than for convective rainfall due to the more evident variability of drop size and number concentration in convective rain. The physical nature of this relationship and the possible mechanisms leading to diverse characteristics in different phases of this heavy rainstorm are discussed. © 2020 Elsevier B.V.
英文关键词Great rainstorm; Northern China; Precipitation microphysics; Raindrop size distribution; Z-R relation
学科领域Drops; Reflection; Remote sensing; Size distribution; Storms; Great rainstorm; Northern China; Precipitation microphysics; Raindrop size distribution; Z-R relation; Rain
语种英语
scopus关键词Drops; Reflection; Remote sensing; Size distribution; Storms; Great rainstorm; Northern China; Precipitation microphysics; Raindrop size distribution; Z-R relation; Rain
来源期刊Atmospheric Research
文献类型期刊论文
条目标识符http://gcip.llas.ac.cn/handle/2XKMVOVA/120406
作者单位Key Laboratory of Cloud-Precipitation Physics and Severe Storms(LACS), Center of Disaster Reduction, Institute of Atmospheric Physics, Chinese Academy of Sciences, Beijing, 100029, China; University of Chinese Academy of Sciences (UCAS), Beijing, 100049, China; Cooperative Institute for Research in the Atmosphere, Colorado State University, Fort Collins, CO 80523, United States; NOAA/Earth System Research Laboratory, Boulder, CO 80305, United States; Beijing Metstar Radar co., Ltd, Beijing, 100085, China
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Luo L.,Xiao H.,Yang H.,et al. Raindrop size distribution and microphysical characteristics of a great rainstorm in 2016 in Beijing, China[J],2020,239.
APA Luo L..,Xiao H..,Yang H..,Chen H..,Guo J..,...&Feng L..(2020).Raindrop size distribution and microphysical characteristics of a great rainstorm in 2016 in Beijing, China.Atmospheric Research,239.
MLA Luo L.,et al."Raindrop size distribution and microphysical characteristics of a great rainstorm in 2016 in Beijing, China".Atmospheric Research 239(2020).
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