基于多尺度小波邊緣檢測的對流降水和閃電分析
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公益性行業科研專項(GYHY200806014)資助


Analysis of Convective Precipitation and Lightning Based on Multiscale Wavelet Edge Detection
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    摘要:

    為準確估測對流降水,提出了多尺度小波邊緣檢測算法,借鑒小波變換的多尺度分析和邊緣檢測原理,對雷達反射率數據進行處理,有效地識別出對流云回波區域,進而反演對流降水,精細化分析其和閃電的相關關系。選取了南京2009年7月6—7日的一次強雷暴降水過程中對流活動較劇烈的180 min為例,對采自南京龍王山雷達站的真實數據進行了算法識別分析,反演得到對流降水,統計6 min時間間隔內的閃電頻數與同期降水進行相關分析,得到該時段中每次閃電所表征的降水量(RPF)的范圍在7.47×106~4.46×107 kg,平

    Abstract:

    Based on the concept of the multiscale wavelet edge detection, an algorithm is presented to process the radar reflectivity data, so to identify convective cloud echoes effectively and retrieve convective precipitation. Taking a severe thunderstorm with heavy precipitations happened in Nanjing between 6 and 7 July 2009 as an example, a case study is conducted, focusing on the 180 minutes with relatively dense lightning flashes and severe precipitation. The convective cloud echo areas are then recognized by means of the multiscale wavelet edge detection algorithm with the radar reflectivity data from Longwang station every 6 minutes. The corresponding convective precipitation is inversed through ZI relation. The lightning flashes in the same 6 minutes are calculated, so the relation between convective precipitation and lightning can be analyzed. Results show that Rain Yields per flash (RPF) ranges from 7.47×106 to 4.46×107  kg, with average value being 1.72×107 kg; the nonlinear curve fitting equation of precipitation intensity and lightning frequency is established.

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徐鳴一,王振會,潘佳文,樊榮,植耀玲,李博,邵程遠.基于多尺度小波邊緣檢測的對流降水和閃電分析[J].氣象科技,2012,40(1):100~106

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  • 收稿日期:2010-07-29
  • 定稿日期:2010-12-13
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  • 在線發布日期: 2012-02-20
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