An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex

<p>Biomass burning aerosol impacts aspects of the atmosphere and Earth system through direct and semi-direct effects, as well as influencing air quality. Despite its importance, the representation of biomass burning aerosol is not always accurate in numerical weather prediction and climate mo...

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Main Authors: A. B. M. Collow, V. Buchard, P. R. Colarco, A. M. da Silva, R. Govindaraju, E. P. Nowottnick, S. Burton, R. Ferrare, C. Hostetler, L. Ziemba
Format: Article
Language:English
Published: Copernicus Publications 2022-12-01
Series:Atmospheric Chemistry and Physics
Online Access:https://acp.copernicus.org/articles/22/16091/2022/acp-22-16091-2022.pdf
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author A. B. M. Collow
A. B. M. Collow
V. Buchard
V. Buchard
P. R. Colarco
A. M. da Silva
R. Govindaraju
R. Govindaraju
E. P. Nowottnick
S. Burton
R. Ferrare
C. Hostetler
L. Ziemba
author_facet A. B. M. Collow
A. B. M. Collow
V. Buchard
V. Buchard
P. R. Colarco
A. M. da Silva
R. Govindaraju
R. Govindaraju
E. P. Nowottnick
S. Burton
R. Ferrare
C. Hostetler
L. Ziemba
author_sort A. B. M. Collow
collection DOAJ
description <p>Biomass burning aerosol impacts aspects of the atmosphere and Earth system through direct and semi-direct effects, as well as influencing air quality. Despite its importance, the representation of biomass burning aerosol is not always accurate in numerical weather prediction and climate models or reanalysis products. Using observations collected as part of the Cloud, Aerosol and Monsoon Processes Philippines Experiment (CAMP<span class="inline-formula"><sup>2</sup></span>Ex) in August through October of 2019, aerosol concentration and optical properties are evaluated within the Goddard Earth Observing System (GEOS) and its underlying aerosol module, GOCART. In the operational configuration, GEOS assimilates aerosol optical depth observations at 550 nm from AERONET and MODIS to constrain aerosol fields. Particularly for biomass burning aerosol, without the assimilation of aerosol optical depth, aerosol extinction is underestimated compared to observations collected in the Philippines region during the CAMP<span class="inline-formula"><sup>2</sup></span>Ex campaign. The assimilation process adds excessive amounts of carbon to account for the underestimated extinction, resulting in positive biases in the mass of black and organic carbon, especially within the boundary layer, relative to in situ observations from the Langley Aerosol Research Group Experiment. Counteracting this, GEOS is deficient in sulfate and nitrate aerosol just above the boundary layer. Aerosol extinction within GEOS is a function of the mass of different aerosol species, the ambient relative humidity, the assumed spectral optical properties, and particle size distribution per species. The relationship between dry and ambient extinction in GEOS reveals that hygroscopic growth is too high within the model for biomass burning aerosol. An additional concern lies in the assumed particle size distribution for GEOS, which has a single mode radius that is too small for organic carbon. Variability in the observed particle size distribution for biomass burning aerosol within a single flight also illuminates the fact that a single assumed particle size distribution is not sufficient and that for a proper representation, a more advanced aerosol module within GEOS may be necessary.</p>
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spelling doaj.art-adad619e31d44678ab5c41c7ba77c41a2022-12-22T10:08:07ZengCopernicus PublicationsAtmospheric Chemistry and Physics1680-73161680-73242022-12-0122160911610910.5194/acp-22-16091-2022An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>ExA. B. M. Collow0A. B. M. Collow1V. Buchard2V. Buchard3P. R. Colarco4A. M. da Silva5R. Govindaraju6R. Govindaraju7E. P. Nowottnick8S. Burton9R. Ferrare10C. Hostetler11L. Ziemba12GESTAR II, University of Maryland Baltimore County, Baltimore, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USAGESTAR II, University of Maryland Baltimore County, Baltimore, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USAScience Systems and Applications, Inc., Lanham, Maryland, USANASA Goddard Space Flight Center, Greenbelt, Maryland, USANASA Langley Research Center, Hampton, Virginia, USANASA Langley Research Center, Hampton, Virginia, USANASA Langley Research Center, Hampton, Virginia, USANASA Langley Research Center, Hampton, Virginia, USA<p>Biomass burning aerosol impacts aspects of the atmosphere and Earth system through direct and semi-direct effects, as well as influencing air quality. Despite its importance, the representation of biomass burning aerosol is not always accurate in numerical weather prediction and climate models or reanalysis products. Using observations collected as part of the Cloud, Aerosol and Monsoon Processes Philippines Experiment (CAMP<span class="inline-formula"><sup>2</sup></span>Ex) in August through October of 2019, aerosol concentration and optical properties are evaluated within the Goddard Earth Observing System (GEOS) and its underlying aerosol module, GOCART. In the operational configuration, GEOS assimilates aerosol optical depth observations at 550 nm from AERONET and MODIS to constrain aerosol fields. Particularly for biomass burning aerosol, without the assimilation of aerosol optical depth, aerosol extinction is underestimated compared to observations collected in the Philippines region during the CAMP<span class="inline-formula"><sup>2</sup></span>Ex campaign. The assimilation process adds excessive amounts of carbon to account for the underestimated extinction, resulting in positive biases in the mass of black and organic carbon, especially within the boundary layer, relative to in situ observations from the Langley Aerosol Research Group Experiment. Counteracting this, GEOS is deficient in sulfate and nitrate aerosol just above the boundary layer. Aerosol extinction within GEOS is a function of the mass of different aerosol species, the ambient relative humidity, the assumed spectral optical properties, and particle size distribution per species. The relationship between dry and ambient extinction in GEOS reveals that hygroscopic growth is too high within the model for biomass burning aerosol. An additional concern lies in the assumed particle size distribution for GEOS, which has a single mode radius that is too small for organic carbon. Variability in the observed particle size distribution for biomass burning aerosol within a single flight also illuminates the fact that a single assumed particle size distribution is not sufficient and that for a proper representation, a more advanced aerosol module within GEOS may be necessary.</p>https://acp.copernicus.org/articles/22/16091/2022/acp-22-16091-2022.pdf
spellingShingle A. B. M. Collow
A. B. M. Collow
V. Buchard
V. Buchard
P. R. Colarco
A. M. da Silva
R. Govindaraju
R. Govindaraju
E. P. Nowottnick
S. Burton
R. Ferrare
C. Hostetler
L. Ziemba
An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
Atmospheric Chemistry and Physics
title An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
title_full An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
title_fullStr An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
title_full_unstemmed An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
title_short An evaluation of biomass burning aerosol mass, extinction, and size distribution in GEOS using observations from CAMP<sup>2</sup>Ex
title_sort evaluation of biomass burning aerosol mass extinction and size distribution in geos using observations from camp sup 2 sup ex
url https://acp.copernicus.org/articles/22/16091/2022/acp-22-16091-2022.pdf
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