Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis

We present the first box model simulation results aimed at identification of possible effects of the atmospheric photochemical evolution of the organic component of biomass burning (BB) aerosol on the aerosol radiative forcing (ARF) and its efficiency (ARFE). The simulations of the dynamics of the o...

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Main Authors: Tatiana B. Zhuravleva, Ilmir M. Nasrtdinov, Igor B. Konovalov, Nikolai A. Golovushkin, Matthias Beekmann
Format: Article
Language:English
Published: MDPI AG 2021-11-01
Series:Atmosphere
Subjects:
Online Access:https://www.mdpi.com/2073-4433/12/12/1555
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author Tatiana B. Zhuravleva
Ilmir M. Nasrtdinov
Igor B. Konovalov
Nikolai A. Golovushkin
Matthias Beekmann
author_facet Tatiana B. Zhuravleva
Ilmir M. Nasrtdinov
Igor B. Konovalov
Nikolai A. Golovushkin
Matthias Beekmann
author_sort Tatiana B. Zhuravleva
collection DOAJ
description We present the first box model simulation results aimed at identification of possible effects of the atmospheric photochemical evolution of the organic component of biomass burning (BB) aerosol on the aerosol radiative forcing (ARF) and its efficiency (ARFE). The simulations of the dynamics of the optical characteristics of the organic aerosol (OA) were performed using a simple parameterization developed within the volatility basis set framework and adapted to simulate the multiday BB aerosol evolution in idealized isolated smoke plumes from Siberian fires (without dilution). Our results indicate that the aerosol optical depth can be used as a good proxy for studying the effect of the OA evolution on the ARF, but variations in the scattering and absorbing properties of BB aerosol can also affect its radiative effects, as evidenced by variations in the ARFE. Changes in the single scattering albedo (SSA) and asymmetry factor, which occur as a result of the BB OA photochemical evolution, may either reduce or enhance the ARFE as a result of their competing effects, depending on the initial concentration OA, the ratio of black carbon to OA mass concentrations and the aerosol photochemical age in a complex way. Our simulation results also reveal that (1) the ARFE at the top of the atmosphere is not significantly affected by the OA oxidation processes compared to the ARFE at the bottom of the atmosphere, and (2) the dependence of ARFE in the atmospheric column and on the BB aerosol photochemical ages almost mirrors the corresponding dependence of SSA.
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spelling doaj.art-73c9789d619946d0b09f21b09dbeada32023-11-23T03:45:19ZengMDPI AGAtmosphere2073-44332021-11-011212155510.3390/atmos12121555Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model AnalysisTatiana B. Zhuravleva0Ilmir M. Nasrtdinov1Igor B. Konovalov2Nikolai A. Golovushkin3Matthias Beekmann4V.E. Zuev Institute of Atmospheric Optics SB RAS, Academician Zuev Square, 1, 634055 Tomsk, RussiaV.E. Zuev Institute of Atmospheric Optics SB RAS, Academician Zuev Square, 1, 634055 Tomsk, RussiaInstitute of Applied Physics of the Russian Academy of Sciences, 46 Ul’yanov Str., 603950 Nizhny Novgorod, RussiaInstitute of Applied Physics of the Russian Academy of Sciences, 46 Ul’yanov Str., 603950 Nizhny Novgorod, RussiaLaboratoire Inter-Universitaire des Systèmes Atmosphériques (LISA), CNRS, 75016 Paris, FranceWe present the first box model simulation results aimed at identification of possible effects of the atmospheric photochemical evolution of the organic component of biomass burning (BB) aerosol on the aerosol radiative forcing (ARF) and its efficiency (ARFE). The simulations of the dynamics of the optical characteristics of the organic aerosol (OA) were performed using a simple parameterization developed within the volatility basis set framework and adapted to simulate the multiday BB aerosol evolution in idealized isolated smoke plumes from Siberian fires (without dilution). Our results indicate that the aerosol optical depth can be used as a good proxy for studying the effect of the OA evolution on the ARF, but variations in the scattering and absorbing properties of BB aerosol can also affect its radiative effects, as evidenced by variations in the ARFE. Changes in the single scattering albedo (SSA) and asymmetry factor, which occur as a result of the BB OA photochemical evolution, may either reduce or enhance the ARFE as a result of their competing effects, depending on the initial concentration OA, the ratio of black carbon to OA mass concentrations and the aerosol photochemical age in a complex way. Our simulation results also reveal that (1) the ARFE at the top of the atmosphere is not significantly affected by the OA oxidation processes compared to the ARFE at the bottom of the atmosphere, and (2) the dependence of ARFE in the atmospheric column and on the BB aerosol photochemical ages almost mirrors the corresponding dependence of SSA.https://www.mdpi.com/2073-4433/12/12/1555biomass burningorganic aerosolmicrophysical modelvolatility basis setMie theory calculationsradiative transfer model
spellingShingle Tatiana B. Zhuravleva
Ilmir M. Nasrtdinov
Igor B. Konovalov
Nikolai A. Golovushkin
Matthias Beekmann
Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
Atmosphere
biomass burning
organic aerosol
microphysical model
volatility basis set
Mie theory calculations
radiative transfer model
title Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
title_full Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
title_fullStr Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
title_full_unstemmed Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
title_short Impact of the Atmospheric Photochemical Evolution of the Organic Component of Biomass Burning Aerosol on Its Radiative Forcing Efficiency: A Box Model Analysis
title_sort impact of the atmospheric photochemical evolution of the organic component of biomass burning aerosol on its radiative forcing efficiency a box model analysis
topic biomass burning
organic aerosol
microphysical model
volatility basis set
Mie theory calculations
radiative transfer model
url https://www.mdpi.com/2073-4433/12/12/1555
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