M. A. Sviridenkov

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Single-scattering albedo ω is one of the main parameters determining the climatic effect of the atmospheric aerosol. Two main approaches to ω retrieval in the atmospheric column from ground-based measurements are known. The first is independent determination of the extinction optical thickness τext from transmission measurements and scattering optical(More)
This paper presents a method to retrieve the particle size distribution function from the data of vertical lidar sensing. We have used 462 data models obtained at the Zvenigorod AERONET site obtained in 2011-2012. For each laser shot, we considered both fine (with particle sizes in a range from 0.05 to 0.6 μm) and coarse aerosol fractions (from 0.6 to 10(More)
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