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Inter-comparison of lidar and ceilometer retrievals for aerosol and Planetary Boundary Layer profiling over Athens, Greece

机译:比较希腊雅典的气溶胶和行星边界层轮廓的激光雷达和云高仪取回

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摘要

This study presents an inter-comparison of two active remote sensors (lidar and ceilometer) to determine the mixing layer height and structure of the Planetary Boundary Layer (PBL) and to retrieve tropospheric aerosol vertical profiles over Athens, Greece. This inter-comparison was performed under various strongly different aerosol loads/types (urban air pollution, biomass burning and Saharan dust event), implementing two different lidar systems (one portable Raymetrics S.A. lidar system running at 355 nm and one multi-wavelength Raman lidar system running at 355 nm, 532 nm and 1064 nm) and one CL31 Vaisala S.A. ceilometer (running at 910nm). Spectral conversions of the ceilometer's data were performed using the Angstrom exponent estimated by ultraviolet multi-filter radiometer (UV-MFR) measurements. The inter-comparison was based on two parameters: the mixing layer height determined by the presence of the suspended aerosols and the attenuated backscatter coefficient. Additionally, radiosonde data were used to derive the PBL height. In general, a good agreement was found between the ceilometer and the lidar techniques in both inter-compared parameters in the height range from 500 m to 5000 m, while the limitations of each instrument are also examined.
机译:这项研究提出了两个有源遥感器(激光雷达和云高仪)之间的比较,以确定混合层的高度和行星边界层(PBL)的结构,并检索希腊雅典上空的对流层气溶胶垂直剖面。这种比较是在各种气溶胶负载/类型(城市空气污染,生物质燃烧和撒哈拉尘埃事件)下进行的,实施了两种不同的激光雷达系统(一种在355 nm处运行的便携式Raymetrics SA激光雷达系统和一种多波长拉曼激光雷达)系统运行在355 nm,532 nm和1064 nm)和一台CL31 Vaisala SA云高仪(运行在910nm)。使用紫外多滤光片辐射计(UV-MFR)测量估计的埃斯特罗姆指数进行云高仪数据的光谱转换。相互比较基于两个参数:由悬浮气溶胶的存在确定的混合层高度和衰减的反向散射系数。另外,探空仪数据被用来推导PBL高度。通常,在500m至5000m高度范围内的两个相互比较的参数中,云高仪和激光雷达技术之间找到了很好的一致性,同时还检查了每种仪器的局限性。

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