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不同闪电日分布地区气溶胶对闪电活动影响

Effects of Aerosols on Lightning Activity in Regions with Different Diurnal Variations in Lightning

  • 摘要: 本研究基于2010~2018年夏季地闪定位和气溶胶光学厚度(AOD)数据,分析了四川盆地(区域1)和广东地区(区域2)的闪电活动与气溶胶的关系。结果表明,区域1和区域2中AOD与地闪频次之间的关系都随AOD的增加而变化,AOD的阈值分别约为.5和0.3。当AOD低于阈值时,两个区域的地闪频次均随AOD的增加而增加。当AOD高于阈值时,两个区域中地闪频次与AOD的关系均变得离散,但在区域1中,地闪频次整体上仍随AOD的增加而增加,而在区域2中,随着AOD的增加,地闪频次先变化不明显,之后呈现下降的趋势。区域1中闪电活动与气溶胶的关系主要由夜间发生的闪电与气溶胶的关系所决定,而区域2中二者的关系则主要由下午发生的闪电与气溶胶的关系所决定。由于气溶胶的辐射抑制作用在白天更强而在夜间更弱,这可能导致了高气溶胶条件下区域1与区域2中闪电活动与气溶胶的不同关系。此外,区域1和区域2中地闪频次的日分布在各个气溶胶含量条件下分别呈现双峰和单峰的形式,在较高的气溶胶含量条件下,区域1傍晚的峰值和区域2下午的峰值出现时间更迟。

     

    Abstract: This study investigated the relationship between lightning activity and aerosols in the Sichuan Basin (Region 1) and Guangdong region (Region 2) by analyzing 9-year (2010–2018) summer datasets of cloud-to-ground (CG) lightning and aerosol optical depth (AOD) data. The results indicate that AOD and CG lightning flashes in both regions are nonlinearly related, with AOD thresholds of about 0.5 and 0.3, respectively. When AOD is below the threshold, the CG lightning flashes in both regions increase with increasing AOD. When AOD exceeds the thresholds, the relationship between the CG lightning flashes and AOD is scattered in both regions. However, in Region 1, the number of CG lightning flashes still increases overall with increasing AOD. In contrast, in Region 2, the CG lightning flashes initially show no significant change and then decrease with increasing AOD. In Region 1, the relationship between lightning activity and aerosols is primarily determined by the relationship between lightning occurring at night and aerosols. In Region 2, the relationship is mainly determined by the relationship between lightning occurring in the afternoon and aerosols. Because the radiative suppression effect of aerosols is stronger during the day and weaker at night, this may lead to different relationships between lightning activity and aerosols under high aerosol conditions in Region 1 and Region 2.. Furthermore, the diurnal variation of CG lightning flashes in Regions 1 and 2 shows bimodal and unimodal forms, respectively, under various aerosol loading conditions. Under high aerosol loading conditions, the evening peak over Region 1 and the afternoon peak over Region 2 are delayed.

     

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