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海南岛正地闪时空分布特征的分析

Temporal and Spatial Distribution of Positive CG Lightning in Hainan Island

  • 摘要: 采用2010—2019年4~10月海南岛闪电定位数据和相关天气分型资料,对海南岛正地闪的频次和频次占比的年分布、月分布、时分布以及各天气分型影响下时分布的特征进行了分析,结果发现:海南岛4~10月的正地闪占比为4.60%,各年份的总地闪频次、正地闪频次、正地闪占比基本呈正相关关系;4~10月的正地闪频次曲线和总地闪频次曲线同为双峰型,且两条曲线峰值所对应的月份相同,但总地闪频次曲线以5月为主峰、8月为次峰,而正地闪频次曲线则以8月为主峰、5月为次峰,8、9月份的正地闪占比要高于其他月份;当采用整体累加法来分析正地闪的时分布时,正地闪频次曲线和总地闪频次曲线同为单峰型,且两条曲线峰值所对应的时间相同,峰值均出现在16:00~17:00,13:00~19:00正地闪占比呈逐时上升趋势;当采用雷暴过程总地闪频次峰期固定法来分析正地闪时分布时,正地闪频次峰值与总地闪频次峰值所对应的时次一致,高峰期前后2小时内的正地闪占比整体呈上升趋势,在总闪频次峰值期稍有下降,正闪主要发生在总闪频次的高峰期及之后,而负闪主要发生在总闪频次的高峰期及之前.通过对海南岛13:00~19:00三种天气分型的正/负地闪密度空间分布特征的分析,发现三种天气分型的正地闪密度高值区相对于负地闪密度高值区稍偏雷暴移动的下游位置.通过分析三起由正地闪所引起的雷灾个例,其结果显示,正闪引起的雷灾可以出现在雷暴过程的成熟期或消亡期,甚至在层状云条件下也可发生,且雷电流强度大、破坏性强.

     

    Abstract: In our report, based on the data of lightning location and Hainan weather typing from 2010 to 2019 (April to October), the frequency and frequency ratio of positive CG lightning in Hainan Island were analyzed in terms of annual distribution, monthly distribution, temporal distribution and temporal distribution under the influence of different weather types. The results showed that the proportion of positive CG lightning in Hainan Island from April to October is 4.60%, the total CG lightning frequency, positive CG lightning frequency and positive CG lightning proportion in each year are basically positively correlated; positive and total CG lightning frequency curves from April to October are both bimodal, and the peaks of the two curves correspond to the same month, however, the total CG lightning frequency curve show the main peak in May and the secondary peak in August, and positive CG lightning frequency curve show the main peak in August and the secondary peak in May, the proportion of positive CG lightning increase month by month from May to August, the proportion of positive CG lightning in August and September is higher than that in other months; when the global summation method is used to analyze positive CG lightning time distribution, both positive and total CG lightning frequency curves are unimodal, and the time corresponding to the peak of the two curves is the same, the peak values all appeare between 16:00 and 17:00, the proportion of positive CG lightning increased hour by hour from 13:00 to 19:00; when the total CG lightning peak period fixation method is used to analyze the time distribution of positive CG lightning frequency during thunderstorm, the peak value of positive CG lightning frequency and total CG lightning frequency correspond to the same time, the proportion of positive CG lightning generally increases hour by hour. In the peak period of total lightning frequency, the proportion of positive CG lightning decrease slightly, positive CG lightning mainly occurs during and after the peak of total CG lighting frequency, the opposite is occur for negative CG lightning. The spatial distribution characteristics of positive and negative CG lightning density of three weather types in Hainan Island from 13:00 to 19:00 are also analyzed. The results indicated that the high value area of positive CG lightning density is the downstream of the thunderstorm movement compared with the high value area of negative CG lightning density of three weather types. The analysis results of three cases of lightning disaster caused by positive lightning suggested that the lightning disaster caused by positive CG lightning occur in the maturity and extinction period of the thunderstorm process, even under the condition of stratiform cloud, and the lightning current intensity is strong and destructive.

     

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