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首页> 外文期刊>Environmental Research Letters >Stratospheric AOD after the 2011 eruption of Nabro volcano measured by lidars over the Northern Hemisphere
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Stratospheric AOD after the 2011 eruption of Nabro volcano measured by lidars over the Northern Hemisphere

机译:北半球激光雷达测得的2011年纳布罗火山爆发后的平流层AOD

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摘要

Nabro volcano (13.37°N, 41.70°E) in Eritrea erupted on 13 June 2011 generating a layer of sulfate aerosols that persisted in the stratosphere for months. For the first time we report on ground-based lidar observations of the same event from every continent in the Northern Hemisphere, taking advantage of the synergy between global lidar networks such as EARLINET, MPLNET and NDACC with independent lidar groups and satellite CALIPSO to track the evolution of the stratospheric aerosol layer in various parts of the globe. The globally averaged aerosol optical depth (AOD) due to the stratospheric volcanic aerosol layers was of the order of 0.018?±?0.009 at 532?nm, ranging from 0.003 to 0.04. Compared to the total column AOD from the available collocated AERONET stations, the stratospheric contribution varied from 2% to 23% at 532?nm.
机译:厄立特里亚的纳布罗火山(北纬13.37°,东经41.70°)于2011年6月13日爆发,产生了一层硫酸盐气溶胶,并在平流层中维持了数月之久。我们首次报告了北半球各大洲对同一事件的地面激光雷达观测结果,利用了全球激光雷达网络(如EARLINET,MPLNET和NDACC)与独立激光雷达组以及卫星CALIPSO之间的协同作用来跟踪卫星全球各地平流层气溶胶层的演变。由于平流层火山气溶胶层引起的全球平均气溶胶光学深度(AOD)在532nm处约为0.018π±0.009,范围为0.003至0.04。与可用的并置AERONET站的总列AOD相比,在532?nm处,平流层的贡献范围从2%到23%不等。

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