ZDR柱識別方法在海南地區的應用
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海南省自然科學基金項目(421QN372)、海南省氣象局科研項目(hnqxZC202112)資助


Application of ZDR Column Recognition Algorithm on Hainan Island
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    摘要:

    基于雙偏振天氣雷達的相關研究大部分集中在雷達如何識別粒子相態、精細化探測云系垂直結構方面,專門針對差分反射率因子ZDR柱的識別研究相對較少。通過對海南地區對流云系特征進行分析研究,提出一套基于雙偏振雷達探測數據(2020—2021年)的ZDR柱識別方法,結合多源資料對發生在海南地區的2次對流天氣過程展開分析,驗證ZDR柱識別效果。結果表明:①ZDR柱通常在對流云系前中期較為深厚,最大可達0 ℃層以上3~5 km,在空間分布上ZDR柱與雷達徑向速度的輻合有密切關系,其正負徑向速度對的差值與ZDR柱的強弱變化規律呈正相關,并且深厚的ZDR柱較大概率出現在對流云系運動方向的前緣位置,與對流云團雷達反射率因子較大區域(≥50 dBz)有明顯的對應關系;②ZDR柱最大深度的變化趨勢同雷達回波頂高和垂直累計液態水含量有弱相關性,雷達回波頂高和垂直累計液態水含量的變化通常滯后于ZDR柱深度的變化(約12~15 min)。該方法具備識別海南島地區ZDR柱現象的能力,可以在分析強對流天氣過程、人工影響天氣指揮和短臨災害天氣預警等方面發揮應用效益。

    Abstract:

    Currently, most of the researches based on dualpolarization weather radar focus on the way to identify the various phases of particles and detect the vertical structure of the clouds, and the researches on the identification and characteristics of ZDR column are few. In order to strengthen the application of dual-polarization radar in Hainan, the identification algorithm of the ZDR column based on the dual-polarization radar (2020-2021) is proposed according to the characteristics of convective cloud systems on the Hainan Island. Based on the method, combined with multi-sources data, two convective weather processes in Hainan are analyzed and studied to verify the ZDR column. The results show that the algorithm can identify the ZDR column on the Hainan Island; the algorithm could obtain the spatial distribution of the ZDR column in real-time to analyze the convective weather processes, weather modification and short-term disaster warning. The ZDR column is usually deep in the early and middle stages of the convective clouds, and the maximum can reach 3 to 5 km above the 0 ℃ layer; the ZDR column with deeper spatial distribution is more likely to appear in the direction of the convective cloud movement. The position of the leading edge has a corresponding relationship with the area with large radar reflectivity (≥50 dBz), which continues to deepen with the evolution of the clouds. The average ZDR column depth variation trend has a weak correlation with the radar echo top height and the vertical accumulated liquid water content. The changes of the radar echo top height and the vertical accumulated liquid water content usually lag the ZDR column depth (12 to 15 min).

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邢峰華,黃彥彬,李光偉,李思騰,車云飛,毛志遠. ZDR柱識別方法在海南地區的應用[J].氣象科技,2022,50(6):859~869

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  • 收稿日期:2022-02-16
  • 定稿日期:2022-07-08
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  • 在線發布日期: 2022-12-30
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