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江西省一次强暴雨过程雷达回波及闪电特征分析

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利用常规观测资料、赣州探空资料、雷达拼图和闪电资料,对2019年6月9日出现的区域性暴雨过程进行了较为细致的分析。结果发现,1)高空东北冷涡较强,冷性结构明显,暴雨区明显辐散;中层平直气流中多短波槽活动,中高纬为两槽一脊,东部大槽后有冷空气不断向江南输送;低层暴雨区处于切变中、急流前的辐合区,是此次强暴雨过程最主要的环流特征;低层切变线、低空西南急流是此次强暴雨过程的重要天气影响系统。2)暴雨过程中雷达回波主要特征为较强组织性的对流回波群、飑线回波和没有组织性的分散性对流回波,其中飑线回波又表现为4个特征,分别是"弓"状飑线回波、"V"形飑线回波、线状飑线回波和短带组成的飑线回波;飑线回波顶高越高,VIL值越大,对流越强盛,降水强度越大。3)有组织的对流单体回波群容易伴随闪电发生,且较为活跃;"V"形飑线回波中"V"形回波顶部容易出现雷电天气,且雷电密度较大;"弓"状回波飑线上雷电活动更加活跃,且维持时间长;线形飑线回波和由短带回波组成的飑线回波上,雷电活动不明显,这是此次强暴雨天气过程中最主要的雷电活动特征;回波顶高和垂直累积液态水含量(VIL)与闪电的出现和强弱之间有较好的相关性。
Analysis of Radar Echo and Lightning Characteristics of A Severe Rainstorm in Jiangxi Province
This study conducts a detailed analysis of a regional severe rainstorm event that occurred on June 9,2019,using conventional observation data,Ganzhou sonde data,radar mosaic and lightning data.The findings indicate that:1)the upper northeast cold vortex was strong,the cold structure was obvious,and the rainstorm area was obviously divergent;There were many short wave troughs in the middle level straight air flow,and there were two troughs and one ridge in the middle and high latitudes.The cold air was continuously transported to the south of the Yangtze River behind the eastern trough;The low-level rainstorm area was located in the convergence area in front of the shear and jet stream,which was the main circulation feature of the heavy rain process.The low-level shear line and low-level southwest jet were the key weather systems influencing this heavy rainstorm.2)The main characteristics of radar echo during the rainstorm process included strong organized convective echo group,squall line echo and unorganized scattered convective echo.Among them,squall line echo exhibited four characteristics,namely"bow"squall line echo,"V"squall line echo,linear squall line echo and squall line echo composed of short band;The higher the top height of the squall line echo,the greater the VIL value,the stronger the convection,and the greater the precipitation intensity.3)The organized convective cell echo group was easily accompanied by lightning and was relatively active;In the"V"squall line echo,the top of the"V"squall line echo was prone to lightning weather,and the lightning density was high;The lightning activity on the"bow"echo squall line was more active and lasted longer;On the linear squall line echo and the squall line echo composed of short band echo,the lightning activity was not obvious,which was the main lightning activity feature in the heavy rain weather process;There was a good correlation between the echo peak height and vertical accumulated liquid water content(VIL)and the occurrence and strength of lightning.

heavy rainlow-level jetsquall line echoecho top heightvertically accumulating liquid water content

黄琳

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江西省上饶市气象局,334000,江西,上饶

强暴雨 低空急流 飑线回波 回波顶高 垂直累积液态水含量

2024

江西科学
江西省科学院

江西科学

影响因子:0.286
ISSN:1001-3679
年,卷(期):2024.42(6)