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Aerosol closure study by lidar, Sun photometry and airborne optical counters during DAMOCLES field campaign at El Arenosillo sounding station, Spain

机译:在西班牙El Arenosillo探测站的DAMOCLES野战期间,由激光雷达,太阳光度计和机载光学计数器进行的气溶胶封闭研究

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摘要

We present a comparison of aerosol properties derived from in situ and remote sensing instruments during DAMOCLES campaign, aimed at investigating the equivalence between the instrumentation and methodologies employed by several Spanish groups to study atmospheric aerosols at a regional background site. The complete set of instruments available during this closure experiment allowed collecting a valuable high-resolution aerosol measurement data set. The data set was augmented with airborne in situ measurements carried out in order to characterize aerosol particles during the midday of 29 June 2006. This work is focused on aerosol measurements using different techniques of high-quality instruments (ground-based remote sensing and aircraft in situ) and their comparisons to characterize the aerosol vertical profiles. Our results indicate that the variability between the detected aerosol layers was negligible in terms of aerosol optical properties and size distributions. Relative differences in aerosol extinction coefficient profiles were less than 20% at 355 and 532 nm and less than 30% at 1064 nm, in the region with high aerosol concentration. Absolute differences in aerosol optical depth (AOD) were below 0.01 at 532 and 1064 nm and less than 0.02 at 355 nm, less than the uncertainties assumed in the AOD obtained from elastic lidar. Columnar values of the lidar ratio revealed some discrepancies with respect to the in situ aircraft measurements, caused fundamentally by the lack of information in the lowest part of the boundary layer.
机译:我们在DAMOCLES运动期间提出了从现场和遥感仪器获得的气溶胶特性的比较,旨在调查几个西班牙小组在区域背景站点研究大气气溶胶所使用的仪器和方法之间的等效性。在该封闭实验期间可使用的全套仪器可以收集有价值的高分辨率气溶胶测量数据集。为了在2006年6月29日中午对气溶胶颗粒进行表征,对飞机进行了原位测量,以增强数据集。这项工作的重点是使用不同质量的仪器(地面遥感和航空器原位)及其比较,以表征气溶胶垂直剖面。我们的结果表明,在气溶胶光学特性和尺寸分布方面,检测到的气溶胶层之间的差异可以忽略不计。在气溶胶浓度高的区域,气溶胶消光系数曲线的相对差异在355和532 nm处小于20%,在1064 nm处小于30%。气溶胶光学深度(AOD)的绝对差在532和1064 nm处小于0.01,在355 nm处小于0.02,小于从弹性激光雷达获得的AOD中的不确定性。激光雷达比的柱状值揭示了就地飞机测量而言的一些差异,这主要是由于边界层最下部缺乏信息。

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