Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine

International audience ReactivehalogensplayaprominentroleintheatmosphericchemistryoftheArcticduringspringtime. Field measurements and modeling studies suggest that halogens are emitted into the atmosphere from snowpack and reactions on wind-blown snow-sourced aerosols. The relative importance of sno...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Swanson, William, F., Holmes, Chris, D., Simpson, William, R., Confer, Kaitlyn, Marelle, Louis, Thomas, Jennie, L., Jaeglé, Lyatt, Alexander, Becky, Zhai, Shuting, Chen, Qianjie, Wang, Xuan, Sherwen, Tomás
Other Authors: Department of Chemistry and Biochemistry Fairbanks, University of Alaska Fairbanks (UAF), Geophysical Institute Fairbanks, Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU, Florida State University Tallahassee (FSU), Department of Atmospheric Sciences Seattle, University of Washington Seattle, Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS), Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS), Department of Civil and Environmental Engineering Hong Kong (CEE), The Hong Kong Polytechnic University Hong Kong (POLYU), School of Energy and Environment Hong Kong, City University of Hong Kong Hong Kong (CUHK), National Centre for Atmospheric Science York (NCAS), University of York York, UK, Department of Chemistry York, UK
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2022
Subjects:
Online Access:https://insu.hal.science/insu-03578658
https://insu.hal.science/insu-03578658v2/document
https://insu.hal.science/insu-03578658v2/file/acp-22-14467-2022.pdf
https://doi.org/10.5194/acp-22-14467-2022
id ftsorbonneuniv:oai:HAL:insu-03578658v2
record_format openpolar
institution Open Polar
collection HAL Sorbonne Université
op_collection_id ftsorbonneuniv
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Swanson, William, F.
Holmes, Chris, D.
Simpson, William, R.
Confer, Kaitlyn
Marelle, Louis
Thomas, Jennie, L.
Jaeglé, Lyatt
Alexander, Becky
Zhai, Shuting
Chen, Qianjie
Wang, Xuan
Sherwen, Tomás
Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience ReactivehalogensplayaprominentroleintheatmosphericchemistryoftheArcticduringspringtime. Field measurements and modeling studies suggest that halogens are emitted into the atmosphere from snowpack and reactions on wind-blown snow-sourced aerosols. The relative importance of snowpack and blowing snow sources is still debated, both at local scales and regionally throughout the Arctic. To understand the implications of these halogen sources on a pan-Arctic scale, we simulate Arctic reactive bromine chemistry in the atmospheric chemical transport model GEOS-Chem. Two mechanisms are included: (1) a blowing snow sea salt aerosol formation mechanism and (2) a snowpack mechanism assuming uniform molecular bromine production from all snow surfaces. We compare simulations including neither mechanism, each mechanism individually, and both mechanisms to examine conditions where one process may dominate or the mechanisms may interact. We compare the models using these mechanisms to observations of bromine monoxide (BrO) derived from multiple- axis differential optical absorption spectroscopy (MAX-DOAS) instruments on O-Buoy platforms on the sea ice and at a coastal site in Utqiag ̇vik, Alaska, during spring 2015. Model estimations of hourly and monthly average BrO are improved by assuming a constant yield of 0.1 % molecular bromine from all snowpack surfaces on ozone deposition. The blowing snow aerosol mechanism increases modeled BrO by providing more bromide-rich aerosol surface area for reactive bromine recycling. The snowpack mechanism led to increased model BrO across the Arctic Ocean with maximum production in coastal regions, whereas the blowing snow aerosol mechanism increases BrO in specific areas due to high surface wind speeds. Our uniform snowpack source has a greater impact on BrO mixing ratios than the blowing snow source. Model results best replicate several features of BrO observations during spring 2015 when using both mechanisms in conjunction, adding evidence that these mechanisms ...
author2 Department of Chemistry and Biochemistry Fairbanks
University of Alaska Fairbanks (UAF)
Geophysical Institute Fairbanks
Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU
Florida State University Tallahassee (FSU)
Department of Atmospheric Sciences Seattle
University of Washington Seattle
Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS)
Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS)
Department of Civil and Environmental Engineering Hong Kong (CEE)
The Hong Kong Polytechnic University Hong Kong (POLYU)
School of Energy and Environment Hong Kong
City University of Hong Kong Hong Kong (CUHK)
National Centre for Atmospheric Science York (NCAS)
University of York York, UK
Department of Chemistry York, UK
format Article in Journal/Newspaper
author Swanson, William, F.
Holmes, Chris, D.
Simpson, William, R.
Confer, Kaitlyn
Marelle, Louis
Thomas, Jennie, L.
Jaeglé, Lyatt
Alexander, Becky
Zhai, Shuting
Chen, Qianjie
Wang, Xuan
Sherwen, Tomás
author_facet Swanson, William, F.
Holmes, Chris, D.
Simpson, William, R.
Confer, Kaitlyn
Marelle, Louis
Thomas, Jennie, L.
Jaeglé, Lyatt
Alexander, Becky
Zhai, Shuting
Chen, Qianjie
Wang, Xuan
Sherwen, Tomás
author_sort Swanson, William, F.
title Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
title_short Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
title_full Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
title_fullStr Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
title_full_unstemmed Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine
title_sort comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to arctic tropospheric reactive bromine
publisher HAL CCSD
publishDate 2022
url https://insu.hal.science/insu-03578658
https://insu.hal.science/insu-03578658v2/document
https://insu.hal.science/insu-03578658v2/file/acp-22-14467-2022.pdf
https://doi.org/10.5194/acp-22-14467-2022
geographic Arctic
Arctic Ocean
geographic_facet Arctic
Arctic Ocean
genre Arctic
Arctic Ocean
Sea ice
Alaska
genre_facet Arctic
Arctic Ocean
Sea ice
Alaska
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://insu.hal.science/insu-03578658
Atmospheric Chemistry and Physics, 2022, 22 (22), pp.14467-14488. ⟨10.5194/acp-22-14467-2022⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-22-14467-2022
insu-03578658
https://insu.hal.science/insu-03578658
https://insu.hal.science/insu-03578658v2/document
https://insu.hal.science/insu-03578658v2/file/acp-22-14467-2022.pdf
doi:10.5194/acp-22-14467-2022
op_rights http://creativecommons.org/licenses/by/
info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/acp-22-14467-2022
container_title Atmospheric Chemistry and Physics
container_volume 22
container_issue 22
container_start_page 14467
op_container_end_page 14488
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spelling ftsorbonneuniv:oai:HAL:insu-03578658v2 2024-06-09T07:43:28+00:00 Comparison of model and ground observations finds snowpack and blowing snow aerosols both contribute to Arctic tropospheric reactive bromine Swanson, William, F. Holmes, Chris, D. Simpson, William, R. Confer, Kaitlyn Marelle, Louis Thomas, Jennie, L. Jaeglé, Lyatt Alexander, Becky Zhai, Shuting Chen, Qianjie Wang, Xuan Sherwen, Tomás Department of Chemistry and Biochemistry Fairbanks University of Alaska Fairbanks (UAF) Geophysical Institute Fairbanks Department of Earth, Ocean and Atmospheric Science Tallahassee (FSU Florida State University Tallahassee (FSU) Department of Atmospheric Sciences Seattle University of Washington Seattle Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes (UGA)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Laboratoire Atmosphères, Milieux, Observations Spatiales (LATMOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Sorbonne Université (SU)-Centre National de la Recherche Scientifique (CNRS) Department of Civil and Environmental Engineering Hong Kong (CEE) The Hong Kong Polytechnic University Hong Kong (POLYU) School of Energy and Environment Hong Kong City University of Hong Kong Hong Kong (CUHK) National Centre for Atmospheric Science York (NCAS) University of York York, UK Department of Chemistry York, UK 2022 https://insu.hal.science/insu-03578658 https://insu.hal.science/insu-03578658v2/document https://insu.hal.science/insu-03578658v2/file/acp-22-14467-2022.pdf https://doi.org/10.5194/acp-22-14467-2022 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-22-14467-2022 insu-03578658 https://insu.hal.science/insu-03578658 https://insu.hal.science/insu-03578658v2/document https://insu.hal.science/insu-03578658v2/file/acp-22-14467-2022.pdf doi:10.5194/acp-22-14467-2022 http://creativecommons.org/licenses/by/ info:eu-repo/semantics/OpenAccess ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://insu.hal.science/insu-03578658 Atmospheric Chemistry and Physics, 2022, 22 (22), pp.14467-14488. ⟨10.5194/acp-22-14467-2022⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2022 ftsorbonneuniv https://doi.org/10.5194/acp-22-14467-2022 2024-05-16T23:53:39Z International audience ReactivehalogensplayaprominentroleintheatmosphericchemistryoftheArcticduringspringtime. Field measurements and modeling studies suggest that halogens are emitted into the atmosphere from snowpack and reactions on wind-blown snow-sourced aerosols. The relative importance of snowpack and blowing snow sources is still debated, both at local scales and regionally throughout the Arctic. To understand the implications of these halogen sources on a pan-Arctic scale, we simulate Arctic reactive bromine chemistry in the atmospheric chemical transport model GEOS-Chem. Two mechanisms are included: (1) a blowing snow sea salt aerosol formation mechanism and (2) a snowpack mechanism assuming uniform molecular bromine production from all snow surfaces. We compare simulations including neither mechanism, each mechanism individually, and both mechanisms to examine conditions where one process may dominate or the mechanisms may interact. We compare the models using these mechanisms to observations of bromine monoxide (BrO) derived from multiple- axis differential optical absorption spectroscopy (MAX-DOAS) instruments on O-Buoy platforms on the sea ice and at a coastal site in Utqiag ̇vik, Alaska, during spring 2015. Model estimations of hourly and monthly average BrO are improved by assuming a constant yield of 0.1 % molecular bromine from all snowpack surfaces on ozone deposition. The blowing snow aerosol mechanism increases modeled BrO by providing more bromide-rich aerosol surface area for reactive bromine recycling. The snowpack mechanism led to increased model BrO across the Arctic Ocean with maximum production in coastal regions, whereas the blowing snow aerosol mechanism increases BrO in specific areas due to high surface wind speeds. Our uniform snowpack source has a greater impact on BrO mixing ratios than the blowing snow source. Model results best replicate several features of BrO observations during spring 2015 when using both mechanisms in conjunction, adding evidence that these mechanisms ... Article in Journal/Newspaper Arctic Arctic Ocean Sea ice Alaska HAL Sorbonne Université Arctic Arctic Ocean Atmospheric Chemistry and Physics 22 22 14467 14488