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THE STATISTIC RELATION BETWEEN LIGHTNING AND CINRAD DOPPLER RADAR ECHOES IN CENTRAL GUANGDONG
作者姓名:彭丽英  万齐林  王谦谦  易燕明
作者单位:PENG Li-ying(Meteorological Bureau of Maoming, Guangdong 525000 China) ; WAN Qi-lin(Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080 China) ; WANG Qian-qian(KLME, NUIST, Nanjing, Jiangsu 210044 China) ; YI Yan-ming(Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080 China) ;
基金项目:Typhoon Research Foundation for Shanghai 2003
摘    要:Based on the CINRAD Doppler radar data in Guangzhou and the lightning data in 2004 by power suppliers of Guangdong, statistical study is done by overlaying lightning’s position on radar’s echo. The result shows the followings. The concentrated period in which more negative lightning occurred at the middle levels (2 – 14 km), where radar echo was moderate (12 – 45 dBz), rather than at the low levels with the weakest echoes or at high levels with the strongest echoes. At levels 3 – 11 km, where the radar echo was between 10 dBz and 35 dBz, the area of negative lightning was much larger in central Guangdong than in the rest of the province. At levels 0.5 – 7 km where the radar echoes were between 44 dBz and 51 dBz, the probability for a point to have negative lightning varies from 0.4 to 0.7.

关 键 词:大气现象  广东  闪电  堆焊

THE STATISTIC RELATION BETWEEN LIGHTNING AND CINRAD DOPPLER RADAR ECHOES IN CENTRAL GUANGDONG
PENG Li-ying,WAN Qi-lin,WANG Qian-qian,YI Yan-ming.THE STATISTIC RELATION BETWEEN LIGHTNING AND CINRAD DOPPLER RADAR ECHOES IN CENTRAL GUANGDONG[J].Journal of Tropical Meteorology,2007,13(2):157-159.
Authors:PENG Li-ying  WAN Qi-lin  WANG Qian-qian  YI Yan-ming
Institution:1. Meteorological Bureau of Maoming, Guangdong 525000 China
2. Guangzhou Institute of Tropical and Marine Meteorology, CMA, Guangzhou 510080 China
3. KLME, NUIST, Nanjing, Jiangsu 210044 China
Abstract:Based on the CINRAD Doppler radar data in Guangzhou and the lightning data in 2004 by power suppliers of Guangdong, statistical study is done by overlaying lightning's position on radar's echo. The result shows the followings. The concentrated period in which more negative lightning occurred at the middle levels (2 - 14 km), where radar echo was moderate (12 - 45 dBz), rather than at the low levels with the weakest echoes or at high levels with the strongest echoes. At levels 3 - 11 km, where the radar echo was between 10 dBz and 35 dBz, the area of negative lightning was much larger in central Guangdong than in the rest of the province. At levels 0.5 - 7 km where the radar echoes were between 44 dBz and 51 dBz,the probability for a point to have negative lightning varies from 0.4 to 0.7.
Keywords:central Guangdong  radar echo  negative cloud-to-ground lightning  overlaying analysis
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