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气象:2023,49(12):1521-1531
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2022年3月14日江西及周边地区冰雹回波特征分析
田白,马中元,陈鲍发,段和平,刘懿枢,岳旭
(江西省气象服务中心,南昌 330096;江西省气象科学研究所,南昌 330046;江西省景德镇市气象局,景德镇 333000;江西省气象灾害防御技术中心,南昌 330046;江西省鹰潭市气象局,鹰潭 335001)
Analysis of Hail Echo Characteristics in Jiangxi and Surrounding Areas on 14 March 2022
TIAN Bai,MA Zhongyuan,CHEN Baofa,DUAN Heping,LIU Yishu,YUE Xu
(Jiangxi Meteorological Service Center, Nanchang 330096;Jiangxi Institute of Meteorological Sciences, Nanchang 330046;Jingdezhen Meteorological Office of Jiangxi Province, Jingdezhen 333000;Jiangxi Meteorological Disaster Prevention Technology Center, Nanchang 330046;Yingtan Meteorological Office of Jiangxi Province, Yingtan 335001)
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投稿时间:2022-12-22    修订日期:2023-08-29
中文摘要: 为更好地开展对江西冰雹天气的监测预警工作,使用MICAPS数据、自动站数据、雷达拼图数据、雷达PUP产品数据、双多普勒雷达反演风场数据、冰雹灾情照片视频和微信冰雹信息反馈等资料,采用天气学、雷达气象学等原理与方法,对2022年3月14日江西及周边省份冰雹回波特征进行分析,结果表明:3月14日,江西及周边省份多地出现冰雹,20个区域站出现≥17.2m·s-1的大风,24个区域站出现≥50.0mm的降水,且雷暴大风和冷空气大风混合出现。200hPa高空出流区、500hPa南支槽和风速切变、850hPa低涡和切变线、地面辐合线和西南倒槽是冰雹天气主要系统;南昌订正后较大的CAPE、较强逆温层、中层干区和低层湿区为冰雹天气发生提供了环境条件。冰雹以超级单体回波为主,有时孤立存在,有时存在于回波群、回波带之中;回波强度≥60 dBz,强回波面积最小≥18km2,最大≥180km2;30~60dBz强回波梯度距离≤6km,具有明显的云砧前伸回波;冰雹回波生命史多数在2h以上。在冰雹回波识别中,垂直积分液态水含量(VIL)是一个很重要的特征。江西冰雹单部雷达VIL在35~60 kg·m-2,雷达拼图上VIL为35~50kg·m-2。在冰雹回波2.5kmCAPPI图上,冰雹回波强度均≥60dBz,最大可达65dBz;在双多普勒雷达反演风场上多数回波中心具有中涡旋结构、侧面辐合风场、南北风场辐合等特征;有些个例风场比较凌乱。上述分析结果为江西冰雹天气的监测预警提供了分析依据。
Abstract:In order to better carry out the monitoring and early warning of hail weather in Jiangxi Province, using MICAPS data, automatic weather station data, radar mosaic data, radar PUP product data, dual-Doppler radar retrieved wind field data, hail disaster photos and videos, and WeChat hail information feedback, as well as principles and methods such as meteorology and radar meteorology, this paper analyzes the characteristics of the hail echoes in Jiangxi and surrounding regions on 14 March 2022. The results show that hails occurred in many places in Jiangxi and surrounding regions, with strong winds of ≥17.2 m·s-1 occurring at 20 regional stations, precipitation ≥50.0 mm occurring at 24 regional stations, and the mixture of thunderstorm gales and cold air. The main impact systems of the hail weather were the 200 hPa outflow zone, the 500 hPa south branch trough and wind speed shear, the 850 hPa low vortex and shear line, the surface convergence line, and the southwest inverted trough. After the correction the larger CAPE value, the stronger inversion layer, the mid-level dry region, and the lower-level wet zone provided ambient conditions for the occurrence of hail weather in Nanchang. Hailstones are mainly composed of supercell echoes, which were sometimes isolated, and sometimes in echo groups and bands. Echo intensity was ≥60 dBz. The minimum strong echo area was ≥18 km2, and the maximum ≥180 km2. The strong echo gradient at a distance of 30-60 dBz was ≤6 km, with obvious cloud anvil forward echo. The life spans of hail echoes were mostly more than 2 hours. In hail echo identification, the vertically integrated liquid (VIL) was a very important feature. The VIL of a single radar of Jiangxi hail was between 35-60 kg·m-2, and the VIL on the radar mosaic was 35-50 kg·m-2. On the CAPPI map of 2.5 km of hail echo, the hail echo intensity was ≥60 dBz, with a maximum of 65 dBz. Most echo centers of dual Doppler radar retrieved wind field had the characteristics of medium vortex structure, lateral convergence wind field, and convergence of north south wind field. Some individual wind fields were relatively messy. The above analysis results could provide an analytical basis for monitoring and early warning of hail weather in Jiangxi.
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基金项目:中国科学院战略性先导科技专项(A类-XDA19040202)、国家自然科学基金项目(41975001、41675029)和江西省科学技术厅2021年省级科技计划项目(20212ABC03A29)共同资助
引用文本:
田白,马中元,陈鲍发,段和平,刘懿枢,岳旭,2023.2022年3月14日江西及周边地区冰雹回波特征分析[J].气象,49(12):1521-1531.
TIAN Bai,MA Zhongyuan,CHEN Baofa,DUAN Heping,LIU Yishu,YUE Xu,2023.Analysis of Hail Echo Characteristics in Jiangxi and Surrounding Areas on 14 March 2022[J].Meteor Mon,49(12):1521-1531.