|
|
X-band dual polarization weather radar MaX-PoI data analysisof hail microphysical processes in Weining County |
Zhang Yan1, Cai Jun1, Chen Lin2, Cai Tong1, Yan Ting1, Ke Liping2 |
1. Weining Meteorological Bureau,Weining 553100; 2. Bijie Meteorological Bureau,Bijie 551700 |
|
|
Abstract The article selects 34 hail cloud units and 26 available hail data observed by the X-band dual polarization weather radar in Weining Yi,Hui,and Miao Autonomous County(referred to as "Weining County") in 2022 for analysis,focusing on the structural characteristics,polarization parameters,and phase distribution characteristics of convective units.By analyzing and comparing with the actual situation,it is concluded that the typical characteristic quantities of convective cell radar echoes are basically consistent.The recognition effects of reflectivity factor,differential reflectivity,and correlation coefficient on meteorological echoes and non meteorological echoes are tested.The accumulated water content zone is mainly distributed within a range of ±2.0 km above the 0 ℃ layer.When the radar echo intensity of convective cells develops from 45 dBZ to above 55 dBZ,hail clouds have the characteristics of rapid development and long duration.The X-band dual polarization weather radar can effectively reflect the types of precipitation particles and conforms to the characteristics of phase distribution,but the transformation of precipitation phase particles in the critical transition zone should be considered.The duration of convective cells and the distribution of accumulated water content zones in Weining County are not conducive to the formation of hail.When the top height of the strong center echo breaks through the -30 ℃ layer,large hail will appear.
|
Received: 27 February 2024
|
|
|
|
|
[1] |
柯莉萍,邹书平,吕静,等.威宁县一次冰雹天气过程的雨滴谱特征分析[J].气象水文海洋仪器,2024,41(6):75-78.
|
[2] |
蔡彤,邹书平,柯莉萍,等.威宁一次降雹过程的雷达回波特征分析[J].气象水文海洋仪器,2024,41(2):70-72,76.
|
[3] |
曾勇,李丽丽,罗雄,等.基于X波段双偏振雷达的贵州威宁一次冰雹过程水成物粒子识别研究[J].中低纬山地气象,2023,47(1):54-62,81.
|
[4] |
曹水,李玮,邹书平,等.威宁冰雹落点时空分布特征[J].中低纬山地气象,2019,43(3):67-70.
|
[5] |
滕林,贺德军,陈军,等.黔东南一次大范围弱冰雹天气过程分析[J].贵州气象,2017,41(5):39-45.
|
[6] |
曾智琳,谌芸,朱克云,等.广东省大冰雹事件的层结特征与融化效应[J].大气科学,2019,43(3):598-617.
|
[7] |
俞小鼎,王迎春,陈明轩,等.新一代天气雷达与强对流天气预警[J].高原气象,2005(3):456-464.
|
[8] |
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.
|
[9] |
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.
|
[10] |
张晰莹,张礼宝,安英玉,等.弱冰雹云雷达回波结构特征分析[J].气象,2008(2):38-42,131-132.
|
[11] |
刁秀广,朱君鉴,黄秀韶,等.VIL和VIL密度在冰雹云判据中的应用[J].高原气象,2008(5):1131-1139.
|
[12] |
徐家骝.冰雹微物理与成雹机制[M].北京: 农业出版社,1979.
|
[13] |
濮文耀,李红斌,宋煜,等.0℃层高度的变化对冰雹融化影响的分析和应用[J].气象,2015,41(8):980-985.
|
[14] |
曹俊武,刘黎平,葛润生.模糊逻辑法在双线偏振雷达识别降水粒子相态中的研究[J].大气科学,2005(5):827-836.
|
[15] |
张培昌,魏鸣,黄兴友,等.双线偏振多普勒天气雷达探测原理与应用[M].北京:气象出版社,2018.
|
[16] |
梅垚,胡志群,黄兴友,等.青藏高原对流云的偏振雷达观测研究[J].气象学报,2018,76(6):1014-1028.
|
[17] |
刁秀广,郭飞燕.2019年8月16日诸城超级单体风暴双偏振参量结构特征分析[J].气象学报,2021,79(2):181-195.
|
[18] |
刘黎平.双线偏振多普勒天气雷达估测混合区降雨和降雹方法的理论研究[J].大气科学,2002(6):761-772.
|
[19] |
曹俊武,刘黎平.双线偏振多普勒天气雷达识别冰雹区方法研究[J].气象,2006(6):13-19.
|
[20] |
刘黎平,钱永甫,王致君.用双线偏振雷达研究云内粒子相态及尺度的空间分布[J].气象学报,1996(5):590-599.
|
|
|
|