Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals

The balance between the cooling and warming effects of aerosol originating from open biomass burning (BB) critically depends on the ratio of its major absorbing and scattering components, such as elemental carbon (EC) and organic carbon (OC), but available direct measurements of this ratio in remote...

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Published in:Atmosphere
Main Authors: Igor Konovalov, Daria Lvova, Matthias Beekmann
Format: Text
Language:English
Published: Multidisciplinary Digital Publishing Institute 2017
Subjects:
Online Access:https://doi.org/10.3390/atmos8070122
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spelling ftmdpi:oai:mdpi.com:/2073-4433/8/7/122/ 2023-08-20T03:59:11+02:00 Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals Igor Konovalov Daria Lvova Matthias Beekmann agris 2017-07-09 application/pdf https://doi.org/10.3390/atmos8070122 EN eng Multidisciplinary Digital Publishing Institute Air Quality https://dx.doi.org/10.3390/atmos8070122 https://creativecommons.org/licenses/by/4.0/ Atmosphere; Volume 8; Issue 7; Pages: 122 biomass burning emissions black carbon carbonaceous aerosol wildfires elemental carbon satellite measurements chemistry transport model Text 2017 ftmdpi https://doi.org/10.3390/atmos8070122 2023-07-31T21:09:48Z The balance between the cooling and warming effects of aerosol originating from open biomass burning (BB) critically depends on the ratio of its major absorbing and scattering components, such as elemental carbon (EC) and organic carbon (OC), but available direct measurements of this ratio in remote regions are limited and rather uncertain. Here, we propose a method to estimate the EC/OC mass ratio in BB aerosol using continuous observations of aerosol optical properties by the Aerosol Robotic Network (AERONET) and apply it to the data from two AERONET sites situated in Siberia. Our method exploits a robust experimental finding (that was reported recently based on laboratory analysis of aerosol from the combustion of wildland fuels) that the single scattering albedo of BB aerosol particles depends linearly on the EC/(EC + OC) mass ratio. We estimated that the mean value of the EC/OC ratio in BB aerosol observed in summer 2012 was 0.036 (±0.009), which is less than the corresponding value (0.061) predicted in our simulations with a chemistry transport model using the emission factors from the Global Fire Emissions Database 4 (GFED4) fire emission inventory. Based on results of our analysis, we propose a parameterization that allows constraining the EC/OC ratio in BB aerosol with available satellite observations of the absorption and extinction aerosol optical depths. Text Aerosol Robotic Network Siberia MDPI Open Access Publishing Atmosphere 8 7 122
institution Open Polar
collection MDPI Open Access Publishing
op_collection_id ftmdpi
language English
topic biomass burning emissions
black carbon
carbonaceous aerosol
wildfires
elemental carbon
satellite measurements
chemistry transport model
spellingShingle biomass burning emissions
black carbon
carbonaceous aerosol
wildfires
elemental carbon
satellite measurements
chemistry transport model
Igor Konovalov
Daria Lvova
Matthias Beekmann
Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
topic_facet biomass burning emissions
black carbon
carbonaceous aerosol
wildfires
elemental carbon
satellite measurements
chemistry transport model
description The balance between the cooling and warming effects of aerosol originating from open biomass burning (BB) critically depends on the ratio of its major absorbing and scattering components, such as elemental carbon (EC) and organic carbon (OC), but available direct measurements of this ratio in remote regions are limited and rather uncertain. Here, we propose a method to estimate the EC/OC mass ratio in BB aerosol using continuous observations of aerosol optical properties by the Aerosol Robotic Network (AERONET) and apply it to the data from two AERONET sites situated in Siberia. Our method exploits a robust experimental finding (that was reported recently based on laboratory analysis of aerosol from the combustion of wildland fuels) that the single scattering albedo of BB aerosol particles depends linearly on the EC/(EC + OC) mass ratio. We estimated that the mean value of the EC/OC ratio in BB aerosol observed in summer 2012 was 0.036 (±0.009), which is less than the corresponding value (0.061) predicted in our simulations with a chemistry transport model using the emission factors from the Global Fire Emissions Database 4 (GFED4) fire emission inventory. Based on results of our analysis, we propose a parameterization that allows constraining the EC/OC ratio in BB aerosol with available satellite observations of the absorption and extinction aerosol optical depths.
format Text
author Igor Konovalov
Daria Lvova
Matthias Beekmann
author_facet Igor Konovalov
Daria Lvova
Matthias Beekmann
author_sort Igor Konovalov
title Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
title_short Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
title_full Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
title_fullStr Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
title_full_unstemmed Estimation of the Elemental to Organic Carbon Ratio in Biomass Burning Aerosol Using AERONET Retrievals
title_sort estimation of the elemental to organic carbon ratio in biomass burning aerosol using aeronet retrievals
publisher Multidisciplinary Digital Publishing Institute
publishDate 2017
url https://doi.org/10.3390/atmos8070122
op_coverage agris
genre Aerosol Robotic Network
Siberia
genre_facet Aerosol Robotic Network
Siberia
op_source Atmosphere; Volume 8; Issue 7; Pages: 122
op_relation Air Quality
https://dx.doi.org/10.3390/atmos8070122
op_rights https://creativecommons.org/licenses/by/4.0/
op_doi https://doi.org/10.3390/atmos8070122
container_title Atmosphere
container_volume 8
container_issue 7
container_start_page 122
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