Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms

Organic compounds from combustion sources such as biomass burning and fossil fuel use are major contributors to the global atmospheric load of aerosols. We analyzed the sensitivity of model-predicted global-scale organic aerosols (OA) to parameters that control primary emissions, photochemical a...

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Main Authors: A. P. Tsimpidi, V. A. Karydis, S. N. Pandis, J. Lelieveld
Format: Article
Language:English
Published: Copernicus Publications 2017-06-01
Series:Atmospheric Chemistry and Physics
Online Access:http://www.atmos-chem-phys.net/17/7345/2017/acp-17-7345-2017.pdf
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author A. P. Tsimpidi
V. A. Karydis
S. N. Pandis
S. N. Pandis
J. Lelieveld
J. Lelieveld
author_facet A. P. Tsimpidi
V. A. Karydis
S. N. Pandis
S. N. Pandis
J. Lelieveld
J. Lelieveld
author_sort A. P. Tsimpidi
collection DOAJ
description Organic compounds from combustion sources such as biomass burning and fossil fuel use are major contributors to the global atmospheric load of aerosols. We analyzed the sensitivity of model-predicted global-scale organic aerosols (OA) to parameters that control primary emissions, photochemical aging, and the scavenging efficiency of organic vapors. We used a computationally efficient module for the description of OA composition and evolution in the atmosphere (ORACLE) of the global chemistry–climate model EMAC (ECHAM/MESSy Atmospheric Chemistry). A global dataset of aerosol mass spectrometer (AMS) measurements was used to evaluate simulated primary (POA) and secondary (SOA) OA concentrations. Model results are sensitive to the emission rates of intermediate-volatility organic compounds (IVOCs) and POA. Assuming enhanced reactivity of semi-volatile organic compounds (SVOCs) and IVOCs with OH substantially improved the model performance for SOA. The use of a hybrid approach for the parameterization of the aging of IVOCs had a small effect on predicted SOA levels. The model performance improved by assuming that freshly emitted organic compounds are relatively hydrophobic and become increasingly hygroscopic due to oxidation.
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spelling doaj.art-d4e44c4cc2b04d60aa55a777eddc44c52022-12-22T02:34:01ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242017-06-01177345736410.5194/acp-17-7345-2017Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanismsA. P. Tsimpidi0V. A. Karydis1S. N. Pandis2S. N. Pandis3J. Lelieveld4J. Lelieveld5Department of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, GermanyDepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, GermanyDepartment of Chemical Engineering, University of Patras, Patras, GreeceDepartment of Chemical Engineering, Carnegie Mellon University, Pittsburgh, PA, USADepartment of Atmospheric Chemistry, Max Planck Institute for Chemistry, Mainz, GermanyEnergy, Environment and Water Research Center, Cyprus Institute, Nicosia, CyprusOrganic compounds from combustion sources such as biomass burning and fossil fuel use are major contributors to the global atmospheric load of aerosols. We analyzed the sensitivity of model-predicted global-scale organic aerosols (OA) to parameters that control primary emissions, photochemical aging, and the scavenging efficiency of organic vapors. We used a computationally efficient module for the description of OA composition and evolution in the atmosphere (ORACLE) of the global chemistry–climate model EMAC (ECHAM/MESSy Atmospheric Chemistry). A global dataset of aerosol mass spectrometer (AMS) measurements was used to evaluate simulated primary (POA) and secondary (SOA) OA concentrations. Model results are sensitive to the emission rates of intermediate-volatility organic compounds (IVOCs) and POA. Assuming enhanced reactivity of semi-volatile organic compounds (SVOCs) and IVOCs with OH substantially improved the model performance for SOA. The use of a hybrid approach for the parameterization of the aging of IVOCs had a small effect on predicted SOA levels. The model performance improved by assuming that freshly emitted organic compounds are relatively hydrophobic and become increasingly hygroscopic due to oxidation.http://www.atmos-chem-phys.net/17/7345/2017/acp-17-7345-2017.pdf
spellingShingle A. P. Tsimpidi
V. A. Karydis
S. N. Pandis
S. N. Pandis
J. Lelieveld
J. Lelieveld
Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
Atmospheric Chemistry and Physics
title Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
title_full Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
title_fullStr Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
title_full_unstemmed Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
title_short Global-scale combustion sources of organic aerosols: sensitivity to formation and removal mechanisms
title_sort global scale combustion sources of organic aerosols sensitivity to formation and removal mechanisms
url http://www.atmos-chem-phys.net/17/7345/2017/acp-17-7345-2017.pdf
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