Frost flower chemical composition during growth and its implications for aerosol production and bromine activation

International audience Frost flowers have been proposed to be the major source of sea-salt aerosol to the atmosphere during polar winter and a source of reactive bromine during polar springtime. However little is known about their bulk chemical composition or microstructure, two important factors th...

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Published in:Journal of Geophysical Research
Main Authors: Alvarez-Aviles, Laura, Simpson, William R., Douglas, Thomas A., Sturm, Matthew, Perovich, Donald, Domine, Florent
Other Authors: Geophysical Institute Fairbanks, University of Alaska Fairbanks (UAF), Department of Chemistry and Biochemistry Fairbanks, ERDC Cold Regions Research and Engineering Laboratory (CRREL), USACE Engineer Research and Development Center (ERDC), Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Observatoire des Sciences de l'Univers de Grenoble (OSUG), Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-00377930
https://hal-insu.archives-ouvertes.fr/insu-00377930/document
https://hal-insu.archives-ouvertes.fr/insu-00377930/file/2008JD010277.pdf
https://doi.org/10.1029/2008JD010277
id ftunivnantes:oai:HAL:insu-00377930v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic Frost flowers
aerosol
Arctic chemistry
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle Frost flowers
aerosol
Arctic chemistry
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Alvarez-Aviles, Laura
Simpson, William R.
Douglas, Thomas A.
Sturm, Matthew
Perovich, Donald
Domine, Florent
Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
topic_facet Frost flowers
aerosol
Arctic chemistry
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience Frost flowers have been proposed to be the major source of sea-salt aerosol to the atmosphere during polar winter and a source of reactive bromine during polar springtime. However little is known about their bulk chemical composition or microstructure, two important factors that may affect their ability to produce aerosols and provide chemically reactive surfaces for exchange with the atmosphere. Therefore, we chemically analyzed 28 samples of frost flowers and parts of frost flowers collected from sea ice off of northern Alaska. Our results support the proposed mechanism for frost flower growth that suggests water vapor deposition forms an ice skeleton that wicks brine present on newly grown sea ice. We measured a high variability in sulfate enrichment factors (with respect to chloride) in frost flowers and seawater from the vicinity of freezing sea ice. The variability in sulfate indicates that mirabilite precipitation (Na2SO4 · 10 H2O) occurs during frost flower growth. Brine wicked up by frost flowers is typically sulfate depleted, in agreement with the theory that frost flowers are related to sulfate-depleted aerosol observed in Antarctica. The bromide enrichment factors we measured in frost flowers are within error of seawater composition, constraining the direct reactive losses of bromide from frost flowers. We combined the chemical composition measurements with temperature observations to create a conceptual model of possible scenarios for frost flower microstructure development.
author2 Geophysical Institute Fairbanks
University of Alaska Fairbanks (UAF)
Department of Chemistry and Biochemistry Fairbanks
ERDC Cold Regions Research and Engineering Laboratory (CRREL)
USACE Engineer Research and Development Center (ERDC)
Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Observatoire des Sciences de l'Univers de Grenoble (OSUG)
Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Alvarez-Aviles, Laura
Simpson, William R.
Douglas, Thomas A.
Sturm, Matthew
Perovich, Donald
Domine, Florent
author_facet Alvarez-Aviles, Laura
Simpson, William R.
Douglas, Thomas A.
Sturm, Matthew
Perovich, Donald
Domine, Florent
author_sort Alvarez-Aviles, Laura
title Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
title_short Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
title_full Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
title_fullStr Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
title_full_unstemmed Frost flower chemical composition during growth and its implications for aerosol production and bromine activation
title_sort frost flower chemical composition during growth and its implications for aerosol production and bromine activation
publisher HAL CCSD
publishDate 2008
url https://hal-insu.archives-ouvertes.fr/insu-00377930
https://hal-insu.archives-ouvertes.fr/insu-00377930/document
https://hal-insu.archives-ouvertes.fr/insu-00377930/file/2008JD010277.pdf
https://doi.org/10.1029/2008JD010277
geographic Arctic
geographic_facet Arctic
genre Antarc*
Antarctica
Arctic
Sea ice
Alaska
genre_facet Antarc*
Antarctica
Arctic
Sea ice
Alaska
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://hal-insu.archives-ouvertes.fr/insu-00377930
Journal of Geophysical Research: Atmospheres, 2008, 113 (D21304), 1 à 10 p. ⟨10.1029/2008JD010277⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2008JD010277
insu-00377930
https://hal-insu.archives-ouvertes.fr/insu-00377930
https://hal-insu.archives-ouvertes.fr/insu-00377930/document
https://hal-insu.archives-ouvertes.fr/insu-00377930/file/2008JD010277.pdf
doi:10.1029/2008JD010277
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2008JD010277
container_title Journal of Geophysical Research
container_volume 113
container_issue D21
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spelling ftunivnantes:oai:HAL:insu-00377930v1 2023-05-15T13:35:39+02:00 Frost flower chemical composition during growth and its implications for aerosol production and bromine activation Alvarez-Aviles, Laura Simpson, William R. Douglas, Thomas A. Sturm, Matthew Perovich, Donald Domine, Florent Geophysical Institute Fairbanks University of Alaska Fairbanks (UAF) Department of Chemistry and Biochemistry Fairbanks ERDC Cold Regions Research and Engineering Laboratory (CRREL) USACE Engineer Research and Development Center (ERDC) Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Observatoire des Sciences de l'Univers de Grenoble (OSUG) Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Université Joseph Fourier - Grenoble 1 (UJF)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Institut national de recherche en sciences et technologies pour l'environnement et l'agriculture (IRSTEA)-Université Savoie Mont Blanc (USMB Université de Savoie Université de Chambéry )-Centre National de la Recherche Scientifique (CNRS)-Centre National de la Recherche Scientifique (CNRS) 2008 https://hal-insu.archives-ouvertes.fr/insu-00377930 https://hal-insu.archives-ouvertes.fr/insu-00377930/document https://hal-insu.archives-ouvertes.fr/insu-00377930/file/2008JD010277.pdf https://doi.org/10.1029/2008JD010277 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2008JD010277 insu-00377930 https://hal-insu.archives-ouvertes.fr/insu-00377930 https://hal-insu.archives-ouvertes.fr/insu-00377930/document https://hal-insu.archives-ouvertes.fr/insu-00377930/file/2008JD010277.pdf doi:10.1029/2008JD010277 info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal-insu.archives-ouvertes.fr/insu-00377930 Journal of Geophysical Research: Atmospheres, 2008, 113 (D21304), 1 à 10 p. ⟨10.1029/2008JD010277⟩ Frost flowers aerosol Arctic chemistry [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2008 ftunivnantes https://doi.org/10.1029/2008JD010277 2023-03-01T02:37:46Z International audience Frost flowers have been proposed to be the major source of sea-salt aerosol to the atmosphere during polar winter and a source of reactive bromine during polar springtime. However little is known about their bulk chemical composition or microstructure, two important factors that may affect their ability to produce aerosols and provide chemically reactive surfaces for exchange with the atmosphere. Therefore, we chemically analyzed 28 samples of frost flowers and parts of frost flowers collected from sea ice off of northern Alaska. Our results support the proposed mechanism for frost flower growth that suggests water vapor deposition forms an ice skeleton that wicks brine present on newly grown sea ice. We measured a high variability in sulfate enrichment factors (with respect to chloride) in frost flowers and seawater from the vicinity of freezing sea ice. The variability in sulfate indicates that mirabilite precipitation (Na2SO4 · 10 H2O) occurs during frost flower growth. Brine wicked up by frost flowers is typically sulfate depleted, in agreement with the theory that frost flowers are related to sulfate-depleted aerosol observed in Antarctica. The bromide enrichment factors we measured in frost flowers are within error of seawater composition, constraining the direct reactive losses of bromide from frost flowers. We combined the chemical composition measurements with temperature observations to create a conceptual model of possible scenarios for frost flower microstructure development. Article in Journal/Newspaper Antarc* Antarctica Arctic Sea ice Alaska Université de Nantes: HAL-UNIV-NANTES Arctic Journal of Geophysical Research 113 D21