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1. 成都信息工程学院大气科学学院
2. 中国气象科学院灾害天气国家重点实验室
3. 中国科学院大气物理研究所中层大气与全球环境探测实验室
4. 西藏自治区气象局气象台
Published:2011
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[1]刘畅,赵鹏国,周筠珺,胡荣,瞿婞.复杂地貌区域内的地闪特征分析[J].高压电器,2011,47(01):22-28.
LIU Chang1, ZHAO Peng-guo1, ZHOU Yun-jun1-4, et al. Characteristics of CG Lightning over Complex Landform Areas[J]. High voltageapparatus, 2011, 47(1): 22-28.
[1]刘畅,赵鹏国,周筠珺,胡荣,瞿婞.复杂地貌区域内的地闪特征分析[J].高压电器,2011,47(01):22-28. DOI: 10.13296/j.1001-1609.hva.2011.01.008.
LIU Chang1, ZHAO Peng-guo1, ZHOU Yun-jun1-4, et al. Characteristics of CG Lightning over Complex Landform Areas[J]. High voltageapparatus, 2011, 47(1): 22-28. DOI: 10.13296/j.1001-1609.hva.2011.01.008.
根据2005-2008年四川雷电监测定位网测得的地闪及该时段内的相关天气资料
运用气候学分析方法
对地处复杂地貌区域内的四川及其周边临近区域的地闪特征进行研究。结果表明:该地区地闪密度分布与其地貌特征有着较为密切的关联性
年平均地闪密度在"川西高原—四川盆地—南部丘陵"依次形成由少到多逐渐增加的分布格局
其最大值超过了1000次/格点
而年平均正地闪密度最大的区域主要位于甘孜州南部的稻城县
其值则超过了50次/格点。在地闪发生的主要季节总地闪频数随纬度变化的最大值出现在北纬30°附近
这与Hadley与Ferrel环流在北纬30°附近形成的下沉气流有关。各年逐月的正地闪占总地闪的百分率分布基本均呈"V"型。在川西高原以东区域的地闪日变化中夜间有两个平均地闪频数的峰值出现
而在川西高原地区只有午后出现一个平均地闪频数的峰值。各雷暴过程中
在冰雹直径3~10mm的区间内
平均正地闪百分比变化与冰雹直径呈正比;最大的平均正地闪百分比30%
与22mm的冰雹直径相对应;16.98%的平均正地闪百分比与10mm的冰雹直径对应
其出现的概率最大超过了37%。
By utilizing data of CG li ghnting from Lightning Monitoring Localization Network in Sichuan province and weather during the 2005-2008
a rather detailed study on characteristics of CG lightning over complex landform areas
which is in Sichuan province and its peripheral regions of China
has been carried out according to climatology analysis methods.Results show as follows.The distribution of CG lightning density correlates closely with the landform in research areas.The average annual density of total CG lightning increases from Western Sichuan Plateau to Sichuan Basin
and then to South hills in turn with the highest value over 1 000/grid
while the area with the highest one of positive CG lightning which is over 50/grid lies in Daocheng county of Ganzi state.The meridional highest frequency of total CG lightning is in the area with the latitude near 30°N in major thunderstorm seasons
and it is induced by subsidence flows of Hadley and Ferrel Cell at 30°N.Monthly percentages of positive CG lightning flashes in total ones for each year basically presents a "V" type.Two peak values of daily CG lightning frequency occur in east of the Western Sichuan Plateau at night
and just one peak value in Western Sichuan Plateau in afternoon.There is positive trend between mean percentages of positive CG lightning flashes and mean hail size as hail diameter increases from 3 to 10 mm.The highest average percentages of positive CG lightning flashes i.e.30% corresponds with the 22 mm hail diameter
and the highest probability density is over 37% for 16.98% percentages of positive CG lightning flashes with 10 mm hail diameter.
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