新余5次冰雹过程雷达回波特征分析

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Abstract Summarizing radar echo characteristics is an effective means to monitor and warn hail weather.Based on the conventional MICAPS weather map,ground meteorological elements,Jiangxi WebGIS radar puzzle CR products and single radar PUP products,this paper analyzes five hail weather processes in Xinyu from 2012 to 2020 by means of statistics and radar echo comparison.The results show that:1)the hail in Xinyu mainly occurs from March to July,and the occurrence time is mostly from afternoon to evening.The main weather types of hail are low trough type and subtropical high edge type.2)The Xinyu hail is mostly produced by super monomer,strong monomer on echo band or super monomer on echo band.The echo center intensity CR of super monomer and super monomer on echo band is more than 60 dBZ.The echo top height is 12~14 km,and the VIL is 60 kg·m².It can be seen from the radial velocity diagram that there are obvious positive and negative velocity pairs with the characteristics of mesocyclone.3)The CR intensity of strong monomer echo is about 5~10 dBZ weaker than that of super monomer echo,and the diameter of hail is also small.The above research results provide a reference basis for the monitoring and early warning of hail in Xinyu.

Key words： Xinyu hail radar puzzle features super monomer

Received: 22 September 2022

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	Li Huanhuan
	Ma Zhongyuan
	Yuan Chun
	Xiao Yun
	Xie Wei

Cite this article:

Li Huanhuan,Ma Zhongyuan,Yuan Chun等. Analysis of radar echo characteristics during five hail events in Xinyu[J]. Meteorological Hydrological and Marine Instrument, 2023, 40(1): 27-31.

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http://www.qxswhy.com/EN/ OR http://www.qxswhy.com/EN/Y2023/V40/I1/27

[1]	俞小鼎,姚秀萍,熊庭南,等.多普勒天气雷达原理与业务应用[M].北京:气象出版社,2006.
[2]	许爱华,孙继松,许东蓓,等.中国中东部强对流天气的天气形势分类和基本要素配置特征[J].气象,2014,40(4):400-411.
[3]	马中元,叶小峰,张瑛,等.江西三类致灾大风天气活动与回波特征分析[J].气象,2011,37(9):1108-1117.
[4]	曹治强,王新.与强对流相联系的云系特征和天气背景[J].应用气象学报,2013,24(3):365-372.
[5]	仇娟娟,何立富.苏沪浙地区短时强降水与冰雹天气分布及物理量特征对比分析[J].气象,2013,39(5):577-584.
[6]	严红梅,梁亮,黄艳,等.金华地区18次冰雹天气的大气环境与雷达回波特征分析[J].暴雨灾害,2019,38(1):48-58.
[7]	廖晓农,俞小鼎,于波.北京盛夏一次罕见的大雹事件分析[J].气象,2008(2):10-17.
[8]	鲁德金,陈钟荣,袁野,等.安徽地区春夏季冰雹云雷达回波特征分析[J].气象,2015,41(9):1104-1110.
[9]	许爱华,马中元,叶小峰.江西8种强对流天气形势与云型特征分析[J].气象,2011,37 (10):1185-1195.
[10]	龙余良,金勇根,刘志萍,等.江西省冰雹气候特征及冰雹灾害研究[J].自然灾害学报,2009,18(1):53-57.
[11]	金米娜,陈云辉,许爱华,等.2013年3月19日江西省冰雹天气成因分析[J].暴雨灾害,2013,32(2):158-166.
[12]	马中元,苏俐敏,谌云,等.一次强飕线及飕前中小尺度系统特征分析[J].气象,2014,40(8):916-929.
[13]	陈鲍发,马中元.江西局地冰雹WebGIS雷达拼图回波特征分析[J].气象与环境科学,2019,42(2):104-114.
[14]	肖云,何金海,许爱华,等.江西省三类强对流天气环境物理量对比分析[J].科学技术与工程,2016,16(14):107-114.
[15]	蒋亚平,张玲玲,奉意杰,等.2018年4月桂西南一次冰雹天气过程诊断分析[J].中低纬山地气象,2021,45(1):40-47.
[16]	罗雄,罗喜平,曾勇,等.贵州省中西部一次冰雹天气过程的涡度收支分析[J].中低纬山地气象,2020,44(4):34-38.
[17]	曹水,邹书平,曾勇,等.一次冰雹云天气过程不同波段雷达回波对比分析[J].中低纬山地气象,2020,44(2):66-70.