Articles | Volume 16, issue 17
https://doi.org/10.5194/acp-16-11433-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/acp-16-11433-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Isotopic constraints on the role of hypohalous acids in sulfate aerosol formation in the remote marine boundary layer
Qianjie Chen
Department of Atmospheric Sciences, University of Washington,
Seattle, WA, USA
Lei Geng
Department of Atmospheric Sciences, University of Washington,
Seattle, WA, USA
now at: Univ. Grenoble-Alpes, LGGE, 38000, Grenoble,
France
now at: CNRS, LGGE, 38000, Grenoble, France
Johan A. Schmidt
Department of Chemistry, University of Copenhagen, Copenhagen,
Denmark
Zhouqing Xie
Institute of Polar Environments, School of Earth and Space Sciences,
University of Science and Technology of China, Hefei, Anhui, China
Hui Kang
Institute of Polar Environments, School of Earth and Space Sciences,
University of Science and Technology of China, Hefei, Anhui, China
Jordi Dachs
Department of Environmental Chemistry, IDAEA-CSIC, IDAEA-CSIC,
Barcelona, Catalunya, Spain
Jihong Cole-Dai
Department of Chemistry and Biochemistry, South Dakota State
University, Brookings, SD, USA
Andrew J. Schauer
Department of Earth and Space Sciences, University of Washington,
Seattle, WA, USA
Madeline G. Camp
Joint Institute for the Study of Atmosphere and Ocean, University of
Washington, Seattle, WA, USA
now at: DSG Solutions, LLC, Shoreline, WA, USA
Becky Alexander
CORRESPONDING AUTHOR
Department of Atmospheric Sciences, University of Washington,
Seattle, WA, USA
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Latest update: 18 Nov 2025
Short summary
The formation mechanisms of sulfate in the marine boundary layer are not well understood, which could result in large uncertainties in aerosol radiative forcing. We measure the oxygen isotopic composition (Δ17O) of sulfate collected in the MBL and analyze with a global transport model. Our results suggest that 33–50 % of MBL sulfate is formed via oxidation of S(IV) by hypohalous acids HOBr / HOCl in the aqueous phase, and the daily-mean HOBr/HOCl concentrations are on the order of 0.01–0.1 ppt.
The formation mechanisms of sulfate in the marine boundary layer are not well understood, which...
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