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Assessment of aerosol's mass concentrations from measured linear particle depolarization ratio (vertically resolved) and simulations
[摘要] Multi-wavelength depolarization Raman lidar measurements from Magurele,Romania are used in this study along with simulated mass-extinctionefficiencies to calculate the mass concentration profiles of differentatmospheric components, due to their different depolarization contribution tothe 532 nm backscatter coefficient. Linear particle depolarization ratio(δpart) was computed using the relative amplification factorand the system-dependent molecular depolarization. The low depolarizingcomponent was considered as urban/smoke, with a mean δpartof 3%, while for the high depolarizing component (mineral dust) a meanδpart of 35% was assumed.

For this study 11 months of lidar measurements were analysed. Two study casesare presented in details: one for a typical Saharan dust aerosol intrusion,10 June 2012 and one for 12 July 2012 when a lofted layer consisting ofbiomass burning smoke extended from 3 to 4.5 km height.

Optical Properties of Aerosols and Clouds software package (OPAC)classification and conversion factors were used to calculate massconcentrations. We found that calibrated depolarization measurements arecritical in distinguishing between smoke-reach aerosol during the winter anddust-reach aerosol during the summer, as well as between elevated aerosollayers having different origins. Good agreement was found between lidarretrievals and DREAM- Dust REgional Atmospheric Model forecasts in cases ofSaharan dust. Our method was also compared against LIRIC (TheLidar/Radiometer Inversion Code) and very small differences were observed.
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