Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow

International audience Snowpacks contain many carbonaceous species that can potentially impact on snow albedo and arctic atmospheric chemistry. During the OASIS field campaign, in March and April 2009, Elemental Carbon (EC), Water insoluble Organic Carbon (WinOC) and Dissolved Organic Carbon (DOC) w...

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Published in:Journal of Geophysical Research: Atmospheres
Main Authors: Voisin, Didier, Jaffrezo, Jean-Luc, Houdier, Stéphan, Barret, Manuel, Cozic, Julie, King, Martin D., France, James L., Reay, Holly J., Grannas, Amanda, Kos, Gregor, Ariya, Parisa A., Beine, Harry J., Domine, Florent
Other Authors: 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), Takuvik International Research Laboratory, Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-03622103
https://hal-insu.archives-ouvertes.fr/insu-03622103/document
https://hal-insu.archives-ouvertes.fr/insu-03622103/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Voisin%20-%20Carbonaceous%20species%20and%20humic%20like%20substances%20HULIS%20in.pdf
https://doi.org/10.1029/2011JD016612
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record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
language English
topic [SDU]Sciences of the Universe [physics]
spellingShingle [SDU]Sciences of the Universe [physics]
Voisin, Didier
Jaffrezo, Jean-Luc
Houdier, Stéphan
Barret, Manuel
Cozic, Julie
King, Martin D.
France, James L.
Reay, Holly J.
Grannas, Amanda
Kos, Gregor
Ariya, Parisa A.
Beine, Harry J.
Domine, Florent
Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
topic_facet [SDU]Sciences of the Universe [physics]
description International audience Snowpacks contain many carbonaceous species that can potentially impact on snow albedo and arctic atmospheric chemistry. During the OASIS field campaign, in March and April 2009, Elemental Carbon (EC), Water insoluble Organic Carbon (WinOC) and Dissolved Organic Carbon (DOC) were investigated in various types of snow: precipitating snows, remobilized snows, wind slabs and depth hoars. EC was found to represent less than 5% of the Total Carbon Content (TCC = EC + WinOC + DOC), whereas WinOC was found to represent an unusual 28 to 42% of TCC. Snow type was used to infer physical processes influencing the evolution of different fractions of DOC. DOC is highest in soil influenced indurated depth hoar layers due to specific wind related formation mechanisms in the early season. Apart from this specific snow type, DOC is found to decrease from precipitating snow to remobilized snow to regular depth hoar. This decrease is interpreted as due to cleaving photochemistry and physical equilibration of the most volatile fraction of DOC. Depending on the relative proportions of diamond dust and fresh snow in the deposition of the seasonal snowpack, we estimate that 31 to 76% of DOC deposited to the snowpack is reemitted back to the boundary layer. Under the assumption that this reemission is purely photochemical, we estimate an average flux of VOC out of the snowpack of 20 to 170 μg C m -2 h -1 . Humic like substances (HULIS), short chain diacids and aldehydes are quantified, and showed to represent altogether a modest (<20%) proportion of DOC, and less than 10% of DOC + WinOC. HULIS optical properties are measured and could be consistent with aged biomass burning or a possible marine source.
author2 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)
Takuvik International Research Laboratory
Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS)
format Article in Journal/Newspaper
author Voisin, Didier
Jaffrezo, Jean-Luc
Houdier, Stéphan
Barret, Manuel
Cozic, Julie
King, Martin D.
France, James L.
Reay, Holly J.
Grannas, Amanda
Kos, Gregor
Ariya, Parisa A.
Beine, Harry J.
Domine, Florent
author_facet Voisin, Didier
Jaffrezo, Jean-Luc
Houdier, Stéphan
Barret, Manuel
Cozic, Julie
King, Martin D.
France, James L.
Reay, Holly J.
Grannas, Amanda
Kos, Gregor
Ariya, Parisa A.
Beine, Harry J.
Domine, Florent
author_sort Voisin, Didier
title Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
title_short Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
title_full Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
title_fullStr Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
title_full_unstemmed Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow
title_sort carbonaceous species and humic like substances (hulis) in arctic snowpack during oasis field campaign in barrow
publisher HAL CCSD
publishDate 2012
url https://hal-insu.archives-ouvertes.fr/insu-03622103
https://hal-insu.archives-ouvertes.fr/insu-03622103/document
https://hal-insu.archives-ouvertes.fr/insu-03622103/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Voisin%20-%20Carbonaceous%20species%20and%20humic%20like%20substances%20HULIS%20in.pdf
https://doi.org/10.1029/2011JD016612
geographic Arctic
geographic_facet Arctic
genre albedo
Arctic
genre_facet albedo
Arctic
op_source ISSN: 2169-897X
EISSN: 2169-8996
Journal of Geophysical Research: Atmospheres
https://hal-insu.archives-ouvertes.fr/insu-03622103
Journal of Geophysical Research: Atmospheres, 2012, 117, 58, p. 73-95. &#x27E8;10.1029/2011JD016612&#x27E9;
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doi:10.1029/2011JD016612
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spelling ftccsdartic:oai:HAL:insu-03622103v1 2023-07-23T04:13:04+02:00 Carbonaceous species and humic like substances (HULIS) in Arctic snowpack during OASIS field campaign in Barrow Voisin, Didier Jaffrezo, Jean-Luc Houdier, Stéphan Barret, Manuel Cozic, Julie King, Martin D. France, James L. Reay, Holly J. Grannas, Amanda Kos, Gregor Ariya, Parisa A. Beine, Harry J. Domine, Florent 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) Takuvik International Research Laboratory Université Laval Québec (ULaval)-Centre National de la Recherche Scientifique (CNRS) 2012 https://hal-insu.archives-ouvertes.fr/insu-03622103 https://hal-insu.archives-ouvertes.fr/insu-03622103/document https://hal-insu.archives-ouvertes.fr/insu-03622103/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Voisin%20-%20Carbonaceous%20species%20and%20humic%20like%20substances%20HULIS%20in.pdf https://doi.org/10.1029/2011JD016612 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2011JD016612 insu-03622103 https://hal-insu.archives-ouvertes.fr/insu-03622103 https://hal-insu.archives-ouvertes.fr/insu-03622103/document https://hal-insu.archives-ouvertes.fr/insu-03622103/file/Journal%20of%20Geophysical%20Research%20Atmospheres%20-%202012%20-%20Voisin%20-%20Carbonaceous%20species%20and%20humic%20like%20substances%20HULIS%20in.pdf BIBCODE: 2012JGRD.117.0R19V doi:10.1029/2011JD016612 http://hal.archives-ouvertes.fr/licences/copyright/ info:eu-repo/semantics/OpenAccess ISSN: 2169-897X EISSN: 2169-8996 Journal of Geophysical Research: Atmospheres https://hal-insu.archives-ouvertes.fr/insu-03622103 Journal of Geophysical Research: Atmospheres, 2012, 117, 58, p. 73-95. &#x27E8;10.1029/2011JD016612&#x27E9; [SDU]Sciences of the Universe [physics] info:eu-repo/semantics/article Journal articles 2012 ftccsdartic https://doi.org/10.1029/2011JD016612 2023-07-02T00:18:47Z International audience Snowpacks contain many carbonaceous species that can potentially impact on snow albedo and arctic atmospheric chemistry. During the OASIS field campaign, in March and April 2009, Elemental Carbon (EC), Water insoluble Organic Carbon (WinOC) and Dissolved Organic Carbon (DOC) were investigated in various types of snow: precipitating snows, remobilized snows, wind slabs and depth hoars. EC was found to represent less than 5% of the Total Carbon Content (TCC = EC + WinOC + DOC), whereas WinOC was found to represent an unusual 28 to 42% of TCC. Snow type was used to infer physical processes influencing the evolution of different fractions of DOC. DOC is highest in soil influenced indurated depth hoar layers due to specific wind related formation mechanisms in the early season. Apart from this specific snow type, DOC is found to decrease from precipitating snow to remobilized snow to regular depth hoar. This decrease is interpreted as due to cleaving photochemistry and physical equilibration of the most volatile fraction of DOC. Depending on the relative proportions of diamond dust and fresh snow in the deposition of the seasonal snowpack, we estimate that 31 to 76% of DOC deposited to the snowpack is reemitted back to the boundary layer. Under the assumption that this reemission is purely photochemical, we estimate an average flux of VOC out of the snowpack of 20 to 170 μg C m -2 h -1 . Humic like substances (HULIS), short chain diacids and aldehydes are quantified, and showed to represent altogether a modest (<20%) proportion of DOC, and less than 10% of DOC + WinOC. HULIS optical properties are measured and could be consistent with aged biomass burning or a possible marine source. Article in Journal/Newspaper albedo Arctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Journal of Geophysical Research: Atmospheres 117 D14 n/a n/a