Liupan Mountain, hail cloud, hail particle size distribution, microphysical characteristics ,"/> <p class="MsoPlainText"> 六盘山区一次非典型冰雹天气过程微物理量特征的分析 <p class="MsoPlainText"> <span></span>
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干旱区地理 ›› 2020, Vol. 43 ›› Issue (2): 299-307.doi: 10.12118/j.issn.1000-6060.2020.02.03

• 气候与水文 • 上一篇    下一篇

六盘山区一次非典型冰雹天气过程微物理量特征的分析

陶涛1，2，张立新1，桑建人2，吕晶晶3，4，聂晶鑫2   

  1. 1 南京信息工程大学大气科学学院，江苏 南京 210044；2 中国气象局旱区特色农业气象灾害监测预警与风险

    管理重点实验室，宁夏 银川 750002；3 中国气象局气溶胶与云降水重点开放实验室，江苏 南京 210044； 4 南京信息工程大学大气物理学院，江苏 南京 210044

  • 收稿日期:2019-03-22 修回日期:2019-06-19 出版日期:2020-03-25 发布日期:2020-03-25
  • 通讯作者: 张立新
  • 作者简介:陶涛（1983-），男，重庆潼南人，大学本科，在职研究生，工程师，研究方向为大气物理及人工影响天气.E-mail:ala.no.4@163.com
  • 基金资助:
    国家自然科学基金重点项目（41775139）资助

A case analysis of microphysical characteristics of atypical hail formation over Liupan Mountain,China

TAO Tao1，2,ZHANG Li-xin1,SANG Jian-ren2,LV Jing-jing3，4,NIE Jing-xin2   

  1. 1 School of Atmospheric Science,Nanjing University of Information Science and Technology,Nanjing 210044,Jiangsu，China;

    2 Key Laboratory of Characteristic Agrometeorological Disaster Monitoring and Early Warning and Risk Management in Arid

    Regions,CMA,Yinchuan 750002,Ningxia,China;

    3 Key Laboratory for AerosolloudPrecipitation of China Meteorological Administration,Nanjing 210044,Jiangsu，China; 4 School of Atmospheric Physics,Nanjing University of Information Science and Technology,Nanjing 210044,Jiangsu，China

  • Received:2019-03-22 Revised:2019-06-19 Online:2020-03-25 Published:2020-03-25

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摘要：

利用地面激光雨滴谱仪捕捉2017年7月14日夜间发生在六盘山区的一次强对流天气降雹过程，其降雨和降雹微物理特征表明：降雹时，粒子各项微物理特征量明显增大，其中数浓度和平均动能通量增幅最为明显，分别增长了6.3倍和13倍。降雹初期，粒径较大的冰雹粒子增长较快，随着能量的释放，对流减弱，粒径较小的冰雹粒子增加较快。Gamma型分布更适合拟合降雹前后的粒子谱。用粒子下落末速度公式V=aDb拟合此次降雹过程中的粒子速度效果很好，相关系数超过0.98，a的变化范围在4.55～5.02之间，b[WTBZ]的变化范围在0.53～0.59之间。

关键词: 六盘山, 冰雹云, 冰雹粒子谱, 微物理特征

Abstract:

Hail is one of the most important destructive weather phenomena in Ningxia Province,China.Its circulation background and spatiotemporal distribution characteristics have been carefully studied by many researchers,but the research on hail with the newest generation of detection equipment is not very clear.This study addressed this gap by examining hail events with measurements of instantaneous precipitation intensity,total number of precipitation particles,cumulative precipitation,visibility,and radar reflectivity that were obtained using a DSG5 laser raindrop spectrometer.The precipitation and microphysical characteristics of hail falling during severe convective weather in the Liupan Mountain area of Ningxia Province on the night of July 14,2017,were systematically analyzed.The results showed as follows: (1) during the hail process,the microphysical characteristics of the precipitation particles increased significantly relative to the baseline.In particular,the number density and mean kinetic energy flux increased to 6.3 and 13 times more than their initial values,respectively.(2) In the early hailing stage,large hail particles grew faster than did smaller particles.However,with the release of energy,convection weakened and hailstones of smaller size increased rapidly.(3) Our data showed that a gammatype distribution was most suitable for fitting the particle distribution characteristics before and after the hail process.(4) Finally,we found that particle velocity during the hail falling process was well fitted by using the particle falling velocity formula V=aDb(R2≥0.98).Fitted to our data,the constant a ranged from 4.55 to 5.02,while b varied from 0.53 to 0.59.

Key words: Liupan Mountain')">

Liupan Mountain, hail cloud, hail particle size distribution, microphysical characteristics