[1]张容菁,李秀昌,彭武坚,等.玉林市“4·19”飑线大风成因及雷达特征分析[J].气象研究与应用,2023,44(03):90-94.[doi:10.19849/j.cnki.CN45-1356/P.2023.3.16]
 ZHANG Rongjing,LI Xiuchang,PENG Wujian,et al.Analysis of the causes of gale and radar characteristics of “4·19”squall line in Yulin[J].Journal of Meteorological Research and Application,2023,44(03):90-94.[doi:10.19849/j.cnki.CN45-1356/P.2023.3.16]
点击复制

玉林市“4·19”飑线大风成因及雷达特征分析()
分享到:

气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第44卷
期数:
2023年03期
页码:
90-94
栏目:
出版日期:
2023-09-15

文章信息/Info

Title:
Analysis of the causes of gale and radar characteristics of “4·19”squall line in Yulin
作者:
张容菁 李秀昌 彭武坚 林确略 陆秋霖
玉林市气象局, 广西 玉林 537000
Author(s):
ZHANG Rongjing LI Xiuchang PENG Wujian LIN Quelue LU Qiulin
Yulin Meteorological Bureau, Guangxi Yulin 537000, China
关键词:
暖区飑线大风环境条件双偏振雷达回波
Keywords:
warm sector squall linestrong windsenvironmental conditionsdual-polarization radar echoes
分类号:
P458.1+23
DOI:
10.19849/j.cnki.CN45-1356/P.2023.3.16
摘要:
利用自动气象站加密和常规观测资料、欧洲中期天气预报中心全球气候第五代大气再分析数据(ERA5)以及SA波段双偏振雷达资料,对2023年4月19日玉林暖区飑线过程进行分析。结果表明:(1)本次飑线过程发生在高空短波槽、低空切变线和地面倒槽锋面影响的环流背景下,是一次湿对流型飑线。(2)中层短波槽的动力作用与低层高温高湿环境配合较好,倒槽中的锋面是触发强对流天气的关键系统,飑线成熟阶段,受中高层短波扰动影响,飑线脱离锋面向暖区快速移动发展。(3)此次暖区飑线过程具有飑中系统的典型特征,飑线后部形成一个冷池,冷池密度流形成强的雷暴出流,造成冷池前部玉林多处出现10级以上大风。(4)雷达回波具有弓状回波、速度模糊、后侧入流缺口等雷暴大风特征,双偏振参量显示ZDR大值区随高度降低,回波均一性较好(CC>0.9),ZDRKDP都可以看到飑线前沿的极大值窄回波带。
Abstract:
Based on data from automatic weather stations, conventional observations, ERA5 reanalysis data, and dual-polarization radar data, the squall line event in the Yulin warm sector that occurred on April 19, 2023 was analyzed. The results show that:(1)The squall line event occurred under the influence of the upper-level shortwave trough, low-level shear line, and surface inverted trough front, indicating it is a moist convective squall line.(2)The dynamic effect of the mid-level shortwave trough, in conjunction with the warm and moist environment in the lower levels, played a significant role. The front within the inverted trough was the key system triggering severe convective weather. During the mature stage of the squall line, influenced by the mid-to upper-level shortwave disturbance, the squall line detached from the front and rapidly developed towards the warm sector.(3)This warm sector squall line event exhibited typical characteristics of a squall system. A cold pool formed behind the squall line, and the density currents associated with the cold pool generated strong thunderstorm outflows. As a result, Yulin experienced gale above magnitude 10 on the Beaufort scale in multiple locations ahead of the cold pool. (4)The radar echoes exhibited characteristics of severe thunderstorm gale, such as bow echoes, velocity aliasing, and rear inflow notches. The dual-polarization parameters showed a decrease in the ZDR(differential reflectivity) maximum values with height, indicating a narrowing echo band with good echo uniformity(CC>0.9). Both ZDR and KDP(specific differential phase) showed the presence of a narrow band of maximum values along the leading edge of the squall line.

参考文献/References:

[1] 章国材,矫梅燕,李延香,等.现代天气预报技术和方法[M].北京:气象出版社,2007:133.
[2] 方翀,林隐静,曹艳察,等.华南地区西风带飑线和台风飑线环境场特征统计对比分析[J].热带气象学报,2017,33(6):965-974.
[3] 叶朗明,伍志方,张华龙,等. 相同季节和相似区域华南两次飑线过程比较分析[J]. 暴雨灾害,2016,35(5):445-454.
[4] 郭弘,林永辉,周淼,等. 华南暖区暴雨中一次飑线的中尺度分析[J]. 暴雨灾害, 2014, 33(2):171-180.
[5] 陈芳丽,窦新英,李明华,等.一次强对流天气过程中尺度对流系统特征分析[J].广东气象,2012,34(2):10-15.
[6] 李影虹,苏文,陈芳丽. 2016年6月4日华南一次罕见强对流天气过程分析[J].广东气象, 2017, 39(4):10-14.
[7] 詹棠,宗淼,郑浩阳. 2013年5月21日广东沿海一次飑线过程的综合分析[J].广东气象, 2015, 37(6):19-22.
[8] 林确略,邓雅倩,陈明璐,等.广西一次槽前型暖区飑线的中尺度分析[J].气象研究与应用,2018,39(1):38-45,155.
[9] 吴福浪,赵成华,陶俞锋.浙江"3·4"暖区飑线环境场和雷达回波特征分析[J].浙江气象,2021,42(4):8-12.
[10] 许可,杜小玲,周文钰,等.贵州一次暖区飑线大风与大冰雹的雷达结构特征分析[J].中低纬山地气象,2021,45(3):65-72.
[11] 吴亚丽. 典型华南暖区暴雨过程(5·7暴雨)的天气学分析及预报研究[D].广州:中山大学,2020.
[12] 聂云,周继先,李习瑾,等.贵州一次暖区飑线过程的环境条件和结构特征[J].干旱气象,2020,38(5):782-793.
[13] 张华龙,肖柳斯,伍志方,等.两次华南飑线卫星亮温特征与强对流天气分析[J].广东气象, 2020,42(2):7-11,16.
[14] 俞小鼎,姚秀萍,熊廷南,等.多普勒天气雷达原理与业务应用[M].北京:气象出版社,2006.
[15] 屈梅芳,俞小鼎,农孟松,等.一次弱垂直风切变环境下飑线发展维持的成因分析[J].暴雨灾害,2021,40(5):466-473.
[16] BROWNING K A. Airflow and Precipitation Trajectories Within Severe Local Storms Which Travel to the Right of the Winds[J]. American Meteorological Society,1964.
[17] 丁治英,夏蘩,高松,等.一次飑线过程中雷达回波的组织结构变化及成因分析[J].热带气象学报,2017,33(3):323-333.
[18] 陈圣劼,刘梅,杨梦兮,等.江苏"4·30"强风雹成因及双偏振雷达特征分析[J].气象科学,2022,42(5):638-649.
[19] 许可,杜小玲,周文钰,等.贵州一次暖区飑线大风与大冰雹的雷达结构特征分析[J].中低纬山地气象,2021,45(3):65-72.
[20] 吴福浪,赵成华,陶俞锋.浙江"3·4"暖区飑线环境场和雷达回波特征分析[J].浙江气象,2021,42(4):8-12.
[21] 郭飞燕,刁秀广,马艳,等.山东一次飑线双偏振结构与地面降水滴谱特征分析[J].气象学报,2023,81(2):328-339.
[22] 陈星登,郭泽勇,张弘豪,等.不同强度云系的双偏振雷达特征[J].气象研究与应用,2021,42(2):19-23.
[23] 杜赛,刘显通,孙皓霆,等.华南一次典型雷暴过程双偏振雷达参量与闪电活动关系研究[J].热带气象学报,2021,37(3):427-438.

相似文献/References:

[1]陆秋霖,黄荣,农孟松,等.2017年4月广西北部一次强对流天气中尺度分析[J].气象研究与应用,2017,38(02):18.
 Lu Qiulin,Huang Rong,Nong Mengsong,et al.Mesoscale analysis of a strong convective weather in northern Guangxi in April 2017[J].Journal of Meteorological Research and Application,2017,38(03):18.
[2]陈伟斌,陈见,赵金彪,等.一次飑线大风天气过程成因分析[J].气象研究与应用,2015,36(01):14.
 Chen Weibin,Chen Jian,Zhao Jinbiao,et al.Causative Analysis of a Squall Line Windy weather Process[J].Journal of Meteorological Research and Application,2015,36(03):14.
[3]覃庆第,邓正良,彭定宇,等.广西近海偏北大风过程极大风速分布特征[J].气象研究与应用,2018,39(02):10.
 Qin Qingdi,Deng Zhengliang,Peng Dingyu,et al.Distribution characteristics of maximum wind speed of northerly gale process in Guangxi offshore[J].Journal of Meteorological Research and Application,2018,39(03):10.
[4]赵飞,潘静,于潇,等.钦州港海域大风日数时空分布特征分析[J].气象研究与应用,2018,39(03):26.
 Zhao Fei,Pan Jing,Yu Xiao,et al.Analysis of temporal and spatial distribution characteristics of gale days in Qinzhou Port[J].Journal of Meteorological Research and Application,2018,39(03):26.
[5]郭彬,卓健,周冬静,等.基于智能计算的广西大风短临预报预警系统的产品检验[J].气象研究与应用,2021,42(01):80.[doi:10.19849/j.cnki.CN45-1356/P.2021.1.14]
 Guo Bin,Zhuo Jian,Zhou Dongjing,et al.Product inspection of Guangxi gale short-term forecast and early warning system based on intelligent computing[J].Journal of Meteorological Research and Application,2021,42(03):80.[doi:10.19849/j.cnki.CN45-1356/P.2021.1.14]
[6]颜佳任,王伟健,张红华,等.2019年江苏两次江淮气旋暴雨大风过程分析[J].气象研究与应用,2021,42(02):83.[doi:10.19849/j.cnki.CN45-1356/P.2021.2.16]
 Yan Jiaren,Wang Weijian,Zhang Honghua,et al.Analysis of two rainstorm and gale processes of Jianghuai cyclone in Jiangsu Province in 2019[J].Journal of Meteorological Research and Application,2021,42(03):83.[doi:10.19849/j.cnki.CN45-1356/P.2021.2.16]
[7]肖志祥,姚才,郑凤琴,等.广西台风与海洋预报服务创新团队研究进展[J].气象研究与应用,2021,42(04):1.[doi:10.19849/j.cnki.CN45-1356/P.2021.4.01]
 Xiao Zhixiang,Yao Cai,Zheng Fengqin,et al.Research progress of Guangxi typhoon and ocean forecast service innovation team[J].Journal of Meteorological Research and Application,2021,42(03):1.[doi:10.19849/j.cnki.CN45-1356/P.2021.4.01]

备注/Memo

备注/Memo:
收稿日期:2023-5-3。
基金项目:广西气象青年人才培养项目(桂气科 2023QN13)、广西气象科技计划指令性项目(桂气科2023ZL11)
作者简介:张容菁(1996-),女,助理工程师,主要从事短期天气预报及环境气象研究工作。E-mail:zorina_rjzhang@foxmail.com
更新日期/Last Update: 1900-01-01