[1]刘昭武,田世芹.黄河三角洲地区冰雹过程雷达特征分析[J].气象研究与应用,2022,43(04):72-78.[doi:10.19849/j.cnki.CN45-1356/P.2022.4.12]
　Liu Zhaowu,Tian Shiqin.Radar characteristic analysis of hail process in the Yellow River Delta area[J].Journal of Meteorological Research and Application,2022,43(04):72-78.[doi:10.19849/j.cnki.CN45-1356/P.2022.4.12]
点击复制

黄河三角洲地区冰雹过程雷达特征分析()
分享到：

气象研究与应用[ISSN:1673-8411/CN:45-1356/P]

卷:
第43卷
期数:
2022年04期
页码:
72-78
栏目:
研究论文
出版日期:
2022-12-15

文章信息/Info

Title:
Radar characteristic analysis of hail process in the Yellow River Delta area
作者:
刘昭武1; 2;  田世芹1; 2
1. 山东省气象防灾减灾重点实验室, 济南 250031;
2. 滨州市气象局, 山东 滨州 256612
Author(s):
Liu Zhaowu1; 2;  Tian Shiqin1; 2
1. Key Laboratory for Meteorological Disaster Prevention and Mitigation of Shandong, Jinan 25003, China;
2. Binzhou Meteorological Bureau, Shangdong Binzhou 256612, China
关键词:
黄河三角洲; 地面降雹; 预警临近指标; 生命史特征
Keywords:
Yellow River Delta; hail on the ground; Early warning approaching indicators; life history characteristics
分类号:
P482
DOI:
10.19849/j.cnki.CN45-1356/P.2022.4.12
摘要:
利用新一代天气雷达产品资料,统计分析了2016-2020年192个黄河三角洲地面降雹个例,从基本反射率因子(R)、垂直积分液态含水量(VIL)、垂直积分液态含水量密度(VILD)特征值等方面归纳出预警临近指标,并应用这些指标分析了2019年5月12日一次局地强对流天气过程。结果表明,风暴单体A3、X3初始回波主要生成于0℃层和-20℃层之间,跃增阶段R、单位体回波厚度平均每个体扫间隔分别增加5.8dBZ、1.5km以上,孕育阶段VIL、强回波最高高度(H45)平均每个体扫间隔分别增加5.6kg·m-2、0.7km以上,且至少出现一次VIL跃增10kg·m-2以上,降雹阶段回波顶高、H45、VIL值迅速减少,具有明显的冰雹云生命史特征;两个风暴单体在孕育、降雹阶段表现出不同的发展演变特点,对冰雹的形成和维持有明显的影响。
Abstract:
Based on the product data of the new-generation of weather radar product data, 192 cases of ground hail in the Yellow River Delta during 2016-2020 were statistically analyzed, and the early warning approaching indicators were summarized from the basic reflectivity factor(R), vertical integrated liquid water content(VIL), and vertical integrated liquid water content density(VILD). A local severe convective weather process on 12 May,2019 was also analysedusing these indicators. The results showed that the initial echoes of storm monomer A3 and X3 were mainly generated between 0℃ and -20℃ layers,the average R and echo height per body sweep interval increased by 5.8 dBZ and 1.8 km or more, respectively in the leapfrog phase. In the breeding stage,the average VIL and strong echo height(H45) per body sweep interval increased by 5.6 kg·m-2 and 0.7 km or more, respectively, and at least once VIL jump increased by more than 10 kg·m-2. In the hail drop stage, the echo height, H45 and VIL value rapidly reduced, with the obvious life history characteristics of hail cloud. The two storm cells showed different development and evolution characteristics during the gestation and hail suppression phases, which had a clear effect on the formation and maintenance of hail.

参考文献/References:

[1] 谢启玉,魏国财.西宁地区冰雹VIL变化特征[J].气象科技,2018,46(3):539-544.
[2] 黄丹萍,梁岱云,陆丽安.南宁冰雹天气类型及预报预警指标[J].气象科技,2020,48(4):554-560.
[3] 刁秀广,张新华,朱君鉴,等.CIMRAD/SA雷达风暴趋势产品在冰雹和大风预警中的应用[J].气象科技,2009,37(2):230-235.
[4] 张磊,张继韫.一次局地强冰雹的多普勒雷达回波特征分析[J].沙漠与绿洲气象,2013,7(4):26-30.
[5] 魏勇,雷微,王存亮,等.石河子地区三次冰雹天气过程的综合分析[J].沙漠与绿洲气象,2013,7(1):21-27.
[6] 希热娜依·铁里瓦尔地,胡素琴,玛依热·艾海提,等.塔里木盆地西缘两次致灾冰雹环境场和雷达特征对比分析[J].沙漠与绿洲气象,2022,16(3):16-23.
[7] 刘昭武,郝茂生,龚佃利.鲁西北地区一次秋季强对流天气的雷达分析[J].气象研究与应用,2020,41(1):79-83.
[8] 李俊河,耿建军,张淅妍,等.2013年北京地区一次强对流天气过程分析[J].沙漠与绿洲气象,2016,10(2):25-30.
[9] 刘希文,李得勤,韦惠红,等.2013年湖北地区两次雷暴大风过程环境及雷达回波特征[J].气象与环境学报,2018,34(1):1-10.
[10] 覃皓,农孟松,赖汉珍,等.2020年"1·24"广西大范围冰雹天气过程分析[J].气象研究与应用,2021,42(1):107-112.
[11] 章国材.强对流天气分析与预报[M].北京:气象出版社,2011:153-156,166.
[12] 彭建东,张丽凡,黄待静.闽北春季冰雹CINRAD雷达产品特征分析[J].气象研究与应用,2018,39(3):48-52.
[13] 王昂生,黄美元,徐乃璋,等.冰雹云物理发展过程的一些研究[J].气象学报,1980,38(1):64-72.
[14] 许焕斌.强对流云物理及其应用[M].北京:气象出版社,2012:10-11.
[15] Smith P L,Myers C G,Orville H D.Radar reflectivity factor calculations in numerical cloud models using bulk parameterization of precipitation[J]. J Appl Meteor,1975(14):1156-165.
[16] 丁帅,肖天贵.延安冰雹多普勒雷达回波特征分析[J].成都信息工程大学学报,2020,35(5):547-553.
[17] 肖辉,吴玉霞,胡朝霞,等.旬邑地区冰雹云的早期识别及数值模拟[J].高原气象,2002,42(1):159-166.

备注/Memo

备注/Memo:
收稿日期:2022-07-15。
基金项目:山东省气象局面上课题(2020sdqxm21)、山东省气象创新团队任务(人工影响天气关键技术创新团队)资助
作者简介:刘昭武(1979-),男,高级工程师,主要从事人工影响天气方面研究。E-mail:lzwbeifeng@126.com
更新日期/Last Update: 1900-01-01