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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 Lightning Diurnal Variations

  • 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的阈值分别为~0.5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和区域2中闪电活动与气溶胶的关系分别由夜间和下午发生的闪电与气溶胶的关系所决定,结合气溶胶的辐射抑制作用在白天更强在夜间更弱,可能导致了高气溶胶含量条件下两个区域闪电活动与气溶胶之间不同的关系。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 there is a non-linear relationship between AOD and CG lightning flashes in regions 1 and 2, with thresholds of~0.5 and~0.3 for AOD, respectively. When AOD is below the threshold, the CG lightning flashes in both regions increases with the increase of AOD. When AOD exceeds the thresholds, the relationship between the CG lightning flashes and AOD becomes scattered in both regions. However, in Region 1, the CG lightning flashes still increases overall with the increase of AOD, while in Region 2, the CG lightning flashes initially shows no significant change and then decreases with the increase of AOD. The relationship between lightning activity and aerosols in regions 1 and 2 is determined by the relationship between lightning and aerosols that occur at night and in the afternoon, respectively. Combined with the radiation suppression effect of aerosols, it is stronger during the day and weaker at night, which may lead to different relationships between lightning activity and aerosols in the two regions under conditions with high aerosol content. In addition, the diurnal variation of CG lightning flashes in regions 1 and 2 shows bimodal and unimodal forms under various aerosol loading, respectively. Under condition with high aerosol loading, the peak in the evening of region 1 and the peak in the afternoon of region 2 appear later.

     

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