Insights into the aging of biomass burning aerosol from satellite observations and 3D atmospheric modeling: Evolution of the aerosol optical properties in Siberian wildfire plumes

International audience Long-range transport of biomass burning (BB) aerosol from regions affected by wildfires is known to have a significant impact on the radiative balance and air quality in receptor regions, including the Arctic. However, the atmospheric evolution of the optical properties of BB...

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Bibliographic Details
Main Authors: Konovalov, Igor, Golovushkin, Nikolai, Beekmann, Matthias, Andreae, Meinrat
Other Authors: Institute of Applied Physics of RAS, Russian Academy of Sciences Moscow (RAS), Laboratoire Interuniversitaire des Systèmes Atmosphériques (LISA (UMR_7583)), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Est Créteil Val-de-Marne - Paris 12 (UPEC UP12)-Centre National de la Recherche Scientifique (CNRS)-Université Paris Cité (UPCité), Biogeochemistry Division, Max-Planck-Institut
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2020
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Online Access:https://hal.science/hal-03032163
https://hal.science/hal-03032163/document
https://hal.science/hal-03032163/file/acp-2020-591_Konovalov_discussion.pdf
https://doi.org/10.5194/acp-2020-591
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Summary:International audience Long-range transport of biomass burning (BB) aerosol from regions affected by wildfires is known to have a significant impact on the radiative balance and air quality in receptor regions, including the Arctic. However, the atmospheric evolution of the optical properties of BB aerosol during the long-range transport events is insufficiently understood, limiting the adequacy of representations of the aerosol processes in chemistry transport and climate models. Here we introduce a framework to infer and interpret changes of the optical properties of BB aerosol from satellite observations of multiple BB plumes. Our framework includes (1) a procedure for analysis of available satellite retrievals of the absorption and extinction aerosol optical depths (AAOD and AOD) and single scattering albedo (SSA) as a function of the BB aerosol photochemical age, and (2) a representation of the AAOD and AOD evolution with a chemistry transport model (CTM) involving a simpli