https://doi.org/10.5194/acp-22-15603-2022">
 

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Creative Commons Attribution 4.0 International License
This work is licensed under a Creative Commons Attribution 4.0 International License.

Authors

Pamela S. Rickly, University of Colorado Boulder
Hongyu Guo, University of Colorado Boulder
Pedro Campuzano-Jost, University of Colorado Boulder
Jose L. Jimenez, University of Colorado Boulder
Glenn M. Wolfe, NASA Goddard Space Flight Center
Ryan Bennett, NASA Ames Research Center
Ilann Bourgeois, University of Colorado, Boulder
John D. Crounse, University of Colorado Boulder
Jack E. Dibb, University of New Hampshire, DurhamFollow
Joshua P. DiGangi, NASA Langley Research Center
Glenn S. Diskin, NASA Langley Research Center
Maximilian Dollner, University of Vienna
Emily M. Gargulinski, NASA Langley Research Center
Samuel R. Hall, National Center for Atmospheric Research
Hannah S. Halliday, Environmental Protection Agency
Thomas F. Hanisco, NASA Goddard Space Flight Center
Reem A. Hannun, NASA Goddard Space Flight Center
Jin Liao, NASA Goddard Space Flight Center
Richard Moore, NASA Langley Research Center
Benjamin A. Nault, Aerodyne Research, Inc.
John B. Nowak, NASA Langley Research Center
Jeff Peischl, University of Colorado, Boulder
Claire E. Robinson, NASA Langley Research Center
Thomas Ryerson, NOAA Chemical Sciences Laboratory
Kevin J. Sanchez, NASA Langley Research Center
Manuel Schöberl, University of Vienna
Amber J. Soja, NASA Langley Research Center
Jason M. St. Clair, NASA Goddard Space Flight Center
Kenneth L. Thornhill, NASA Langley Research Center
Kirk Ullmann, National Center for Atmospheric Research
Paul O. Wennberg, California Institute of Technology
Bernadett Weinzierl, University of Vienna
Elizabeth B. Wiggins, NASA Langley Research Center
Edward L. Winstead, NASA Langley Research Center
Andrew W. Rollins, Chemical Sciences Laboratory, NOAA

Abstract

Fires emit sufficient sulfur to affect local and regional air quality and climate. This study analyzes SO2 emission factors and variability in smoke plumes from US wildfires and agricultural fires, as well as their relationship to sulfate and hydroxymethanesulfonate (HMS) formation. Observed SO2 emission factors for various fuel types show good agreement with the latest reviews of biomass burning emission factors, producing an emission factor range of 0.47–1.2 g SO2 kg−1 C. These emission factors vary with geographic location in a way that suggests that deposition of coal burning emissions and application of sulfur-containing fertilizers likely play a role in the larger observed values, which are primarily associated with agricultural burning. A 0-D box model generally reproduces the observed trends of SO2 and total sulfate (inorganic + organic) in aging wildfire plumes. In many cases, modeled HMS is consistent with the observed organosulfur concentrations. However, a comparison of observed organosulfur and modeled HMS suggests that multiple organosulfur compounds are likely responsible for the observations but that the chemistry of these compounds yields similar production and loss rates as that of HMS, resulting in good agreement with the modeled results. We provide suggestions for constraining the organosulfur compounds observed during these flights, and we show that the chemistry of HMS can allow organosulfur to act as an S(IV) reservoir under conditions of pH > 6 and liquid water content >10−7 g sm−3. This can facilitate long-range transport of sulfur emissions, resulting in increased SO2 and eventually sulfate in transported smoke.

Department

Earth Systems Research Center

Publication Date

12-13-2022

Journal Title

Atmospheric Chemistry and Physics

Publisher

EGU

Digital Object Identifier (DOI)

https://doi.org/10.5194/acp-22-15603-2022

Document Type

Article

Rights

© The Author(s) 2022

Comments

This is an open access article published by EGU in Atmospheric Chemistry and Physics in 2022, available online: https://doi.org/10.5194/acp-22-15603-2022

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