气象与减灾研究2024,Vol.47Issue(3) :163-172.DOI:10.12013/qxyjzyj2024-021

江西中北部地区冰雹过程双偏振雷达特征

Dual-Polarization Radar Characteristics of Hail Events in the Central-Northern Regions of Jiangxi Province

彭恩翔 张帆 曾唯睿 胡怀坚 孙素琴
气象与减灾研究2024,Vol.47Issue(3) :163-172.DOI:10.12013/qxyjzyj2024-021

江西中北部地区冰雹过程双偏振雷达特征

Dual-Polarization Radar Characteristics of Hail Events in the Central-Northern Regions of Jiangxi Province

彭恩翔 1张帆 2曾唯睿 1胡怀坚 1孙素琴3
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作者信息

  • 1. 吉安市气象局,吉安市生态气象重点实验室,江西吉安 343000
  • 2. 赣州市气象局,江西赣州 341000
  • 3. 江西省气象台,江西南昌 330096
  • 折叠

摘要

实际业务中对冰雹大小的判断一直是难点之一,为区分和识别不同尺寸的冰雹,基于地面观测资料和南昌、吉安两部双偏振雷达探测资料,筛选出2021-2024年2-5月44次冰雹事件,统计分析不同尺寸的冰雹在不同高度层的雷达偏振量及其变化,得到江西中北部地区冰雹过程雷达偏振量的阈值特征.结果表明:1)在相同高度层上,冰雹尺寸越大,反射率因子(ZH)的中位数越大,差分反射率因子(ZDR)和相关系数(CC)的中位数越小,其中特大冰雹与小冰雹的ZH中位数差值在近地层和-20 ℃层以上高度层都大于等于10dBZ.2)在融化层以下高度小冰雹的ZDR中位数基本为正值,大冰雹的在多个高度层接近0 dB,特大冰雹的则基本为负值;融化层以下高度特大冰雹的CC值基本小于0.9.3)在-20 ℃层以上高度ZH对冰雹尺寸较敏感,CC和ZDR表现不明显;-20-0 ℃层的ZH和CC对冰雹尺寸较敏感,ZDR表现不明显;融化层以下高度ZH、CC和ZDR对冰雹尺寸均有一定的指示意义.4)结合多类偏振量可以更好地判断冰雹的尺寸大小,冰雹尺寸越大,出现三体散射的概率越高,利用三体散射的偏振特征可有效辅助识别大冰雹.

Abstract

In practical operations,the judgment of hail size has always been one of the challenges.To distinguish and identify hails of different sizes,44 hail events in Jiangxi from February to May during 2021-2024 were selected based on ground obser-vation data and dual-polarization radar data from Nanchang and Ji'an stations.According to the radar polarization values and their variations at different altitude levels for hail of different sizes in the central-northern regions of Jiangxi Province,the threshold characteristics for distinguishing different sizes of hails were obtained.The results showed that:1)At the same alti-tude level,the larger the hail size,the greater the median ZH value,and the smaller the median ZDR value and CC value.The median difference in ZH values between giant hail and small hail were more than or equal to 10 dBZ in both the near-ground lay-er and the altitude layer above-20 ℃ layer.2)The median ZUR value of small hail below the melting layer was generally posi-tive,the median ZDR value of large hail was close to 0 dB at multiple altitude levels,while the median ZDR value of giant hail was generally negative.The CC value of giant hail below the melting layer was typically less than 0.9.3)Above the-20 ℃ layer,ZH was more sensitive to hail size,while CC and ZDR showed less significant variation.Among-20 and 0 ℃ layer,ZH and CC were more sensitive to hail size,while ZDR showed less variation.Below the melting layer,ZH,CC and ZDR all provided certain indications of hail size.4)The size of hails would be better determined by combining multiple types of polarization pa-rameters.The larger the hail size,the higher the probability of TBSS.The polarization feature of TBSS would be used to iden-tify large hail effectively.

关键词

天气雷达/冰雹尺寸/偏振特征/三体散射/温度层高度

Key words

weather radar/hail size/polarization characteristics/TBSS/height of temperature layer

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出版年

2024
气象与减灾研究
江西省气象学会

气象与减灾研究

影响因子:0.881
ISSN:1007-9033
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