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基于S波段双偏振雷达观测的雹暴偏振特征分析
引用本文:潘佳文,高丽,魏鸣,蒋璐璐,蔡菁. 基于S波段双偏振雷达观测的雹暴偏振特征分析[J]. 气象学报, 2021, 79(1): 168-180. DOI: 10.11676/qxxb2021.001
作者姓名:潘佳文  高丽  魏鸣  蒋璐璐  蔡菁
作者单位:海峡气象开放实验室,厦门市气象局,厦门, 361012;台州市气象局,台州, 318000;气象灾害预报预警与评估协同创新中心,南京信息工程大学,南京, 210044;宁波市气象局,宁波, 315012;龙岩市气象局,龙岩, 364000
基金项目:国家自然科学基金(41675029)、福建省自然科学基金(2018J01060)、福建省气象局基层科技专项(2019J06)、福建省气象局开放式研究基金(2020KX01)
摘    要:为了研究雹暴的偏振特征及其在实际业务中的应用,使用S波段双偏振雷达所观测到的46例冰雹数据,对其中反复出现的3种偏振特征:冰雹在各高度层的偏振参数特征、差分反射率因子柱、三体散射偏振特征进行了分析,重点分析了3种偏振特征大、小冰雹事件的差异.结果表明:(1)大冰雹的水平反射率因子中位数要高于小冰雹,二者的水平反射率因子...

关 键 词:双偏振雷达  冰雹  偏振特征
收稿时间:2020-06-09
修稿时间:2020-09-08

Analysis of the polarimetric characteristics of hail storm from S band dual polarization radar observations
PAN Jiawen,GAO Li,WEI Ming,JIANG Lulu,CAI Jing. Analysis of the polarimetric characteristics of hail storm from S band dual polarization radar observations[J]. Acta Meteorologica Sinica, 2021, 79(1): 168-180. DOI: 10.11676/qxxb2021.001
Authors:PAN Jiawen  GAO Li  WEI Ming  JIANG Lulu  CAI Jing
Affiliation:1.Laboratory of Straits Meteorology, Xiamen Meteorological Bureau, Xiamen 361012, China2.Taizhou Meteorological Bureau, Taizhou 318000, China3.Collaborative Innovation Center on Forecast and Evaluation of Meteorological Disasters, NUIST, Nanjing 210044, China4.Ningbo Meteorological Bureau, Ningbo 315012, China5.Longyan Meteorological Bureau, Longyan 364000, China
Abstract:This study aims to investigate the polarimetric radar characteristics of hail storm and application of these characteristics for operational work. A total of 46 hail storm reports that have been observed with the S-band dual-polarization radar are used for this study. Three polarimetric signatures, i.e., the polarimetric variables of hail at various height, Zdr column, the polarimetric TBSS, are repeatedly found in these hail storms and analyzed with the focus on the differences between polarimetric signatures of large and small hails. The study yields the following results: (1) The median value of Zh for large hails is higher than the value for small hails. A significant overlap of the Zh distributions for large and small hails is also present. (2) The variation of polarimetric variables of hail is concentrated below the melting level. Compared with small hails, large hails have lower Zdr and correlation coefficient (CC) values. (3) The maximum height of Zdr column can reach the ?10℃ level in all of the hail storms, while 83% of large hail reports and 46% of small hail reports show that the Zdr column could penetrate the ?20℃ level. (4) The evolution of the Zdr column height is an appropriate index that can reflect the development of the hail storm. During a continuous hail process, the re-development of the Zdr column height occurs earlier than that of the hail storm. It is also found that the peak of Zdr column height usually occurs about 24 min (median value) prior to a large hail report and about 11 min (median value) prior to a small hail report. (5) The polarimetric TBSS is a good indicator for identifying hails aloft, especially when there are other precipitation echoes located radially behind the hail core. In this study, the polarimetric TBSS can be found in all of the large hail reports and in 52% of the small hail reports. 
Keywords:Dual polarization radar  Hail  Polarimetric characteristics
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