Levoglucosan as a specific marker of fire events in Greenland snow

International audience We demonstrate the use of levoglucosan (1,6-anhydro-β-d-glucopyranose) as a source-specific proxy of past fire activity in snow pits and ice cores. Levoglucosan is unambiguously a degradation product derived from cellulose burning at temperatures greater than 300 °C and is wid...

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Published in:Tellus B: Chemical and Physical Meteorology
Main Authors: Kehrwald, Natalie, Zangrando, Roberta, Gabrielli, Paolo, Jaffrezo, Jean-Luc, Boutron, Claude, Barbante, Carlo, Gambaro, Andrea
Other Authors: Department of Environmental Sciences, Informatics and Statistics Venezia, University of Ca’ Foscari Venice, Italy, Institute for the Dynamics of Environmental Processes-National Research Council, School of Earth Sciences, Ohio State University Columbus (OSU), Byrd Polar Research Center, 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), Université Joseph Fourier - Grenoble 1 - UFR Physique, Ingénierie, Terre, Environnement, Mécanique (UJF UFR PhiTEM), Université Joseph Fourier - Grenoble 1 (UJF), Accademia Nazionale dei Lincei, ''Centro Beniamino Segre'', Accademia Nazionale dei Lincei, ''Centro Beniamino Segre'', PIIF-GA-2009-236961 PaleoFire
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2012
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-00845304
https://hal-insu.archives-ouvertes.fr/insu-00845304/document
https://hal-insu.archives-ouvertes.fr/insu-00845304/file/18196-60949-1-PB.pdf
https://doi.org/10.3402/tellusb.v64i0.18196
id ftunivnantes:oai:HAL:insu-00845304v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic biomass burning
levoglucosan
snow
ice core
Greenland
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
spellingShingle biomass burning
levoglucosan
snow
ice core
Greenland
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Kehrwald, Natalie
Zangrando, Roberta
Gabrielli, Paolo
Jaffrezo, Jean-Luc
Boutron, Claude
Barbante, Carlo
Gambaro, Andrea
Levoglucosan as a specific marker of fire events in Greenland snow
topic_facet biomass burning
levoglucosan
snow
ice core
Greenland
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
description International audience We demonstrate the use of levoglucosan (1,6-anhydro-β-d-glucopyranose) as a source-specific proxy of past fire activity in snow pits and ice cores. Levoglucosan is unambiguously a degradation product derived from cellulose burning at temperatures greater than 300 °C and is widely used as a biomass burning marker in aerosol analyses. We analyse samples collected from a 3 m snow pit at Summit, Greenland (72°20′N, 38°45′W; 3270 m a.s.l.), with a known depositional history where biomass burning aerosols were traced from their source in a Canadian smoke plume, through their eastward transport and deposition on the Greenland ice sheet, and their eventual burial by accumulating snow layers. The snow pit levoglucosan profile replicates oxalate concentrations from a known forest fire event, suggesting the applicability of levoglucosan as a marker of past fire activity in snow and by extension in ice cores. However, levoglucosan concentration peaks in the snow pit differ from those of ammonium and potassium, which are traditionally used as biomass burning proxies in snow and ice studies but which incorporate sources other than fire activity. The source specificity of levoglucosan can help determine the past relative contribution of biomass burning aerosols when used in conjunction with other proxies in snow and ice.
author2 Department of Environmental Sciences, Informatics and Statistics Venezia
University of Ca’ Foscari Venice, Italy
Institute for the Dynamics of Environmental Processes-National Research Council
School of Earth Sciences
Ohio State University Columbus (OSU)
Byrd Polar Research Center
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)
Université Joseph Fourier - Grenoble 1 - UFR Physique, Ingénierie, Terre, Environnement, Mécanique (UJF UFR PhiTEM)
Université Joseph Fourier - Grenoble 1 (UJF)
Accademia Nazionale dei Lincei, ''Centro Beniamino Segre''
Accademia Nazionale dei Lincei, ''Centro Beniamino Segre'',
PIIF-GA-2009-236961 PaleoFire
format Article in Journal/Newspaper
author Kehrwald, Natalie
Zangrando, Roberta
Gabrielli, Paolo
Jaffrezo, Jean-Luc
Boutron, Claude
Barbante, Carlo
Gambaro, Andrea
author_facet Kehrwald, Natalie
Zangrando, Roberta
Gabrielli, Paolo
Jaffrezo, Jean-Luc
Boutron, Claude
Barbante, Carlo
Gambaro, Andrea
author_sort Kehrwald, Natalie
title Levoglucosan as a specific marker of fire events in Greenland snow
title_short Levoglucosan as a specific marker of fire events in Greenland snow
title_full Levoglucosan as a specific marker of fire events in Greenland snow
title_fullStr Levoglucosan as a specific marker of fire events in Greenland snow
title_full_unstemmed Levoglucosan as a specific marker of fire events in Greenland snow
title_sort levoglucosan as a specific marker of fire events in greenland snow
publisher HAL CCSD
publishDate 2012
url https://hal-insu.archives-ouvertes.fr/insu-00845304
https://hal-insu.archives-ouvertes.fr/insu-00845304/document
https://hal-insu.archives-ouvertes.fr/insu-00845304/file/18196-60949-1-PB.pdf
https://doi.org/10.3402/tellusb.v64i0.18196
geographic Greenland
geographic_facet Greenland
genre Greenland
ice core
Ice Sheet
genre_facet Greenland
ice core
Ice Sheet
op_source ISSN: 0280-6509
EISSN: 1600-0889
Tellus B - Chemical and Physical Meteorology
https://hal-insu.archives-ouvertes.fr/insu-00845304
Tellus B - Chemical and Physical Meteorology, 2012, 64, pp.18196. ⟨10.3402/tellusb.v64i0.18196⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.3402/tellusb.v64i0.18196
insu-00845304
https://hal-insu.archives-ouvertes.fr/insu-00845304
https://hal-insu.archives-ouvertes.fr/insu-00845304/document
https://hal-insu.archives-ouvertes.fr/insu-00845304/file/18196-60949-1-PB.pdf
doi:10.3402/tellusb.v64i0.18196
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.3402/tellusb.v64i0.18196
container_title Tellus B: Chemical and Physical Meteorology
container_volume 64
container_issue 1
container_start_page 18196
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spelling ftunivnantes:oai:HAL:insu-00845304v1 2023-05-15T16:26:28+02:00 Levoglucosan as a specific marker of fire events in Greenland snow Kehrwald, Natalie Zangrando, Roberta Gabrielli, Paolo Jaffrezo, Jean-Luc Boutron, Claude Barbante, Carlo Gambaro, Andrea Department of Environmental Sciences, Informatics and Statistics Venezia University of Ca’ Foscari Venice, Italy Institute for the Dynamics of Environmental Processes-National Research Council School of Earth Sciences Ohio State University Columbus (OSU) Byrd Polar Research Center 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) Université Joseph Fourier - Grenoble 1 - UFR Physique, Ingénierie, Terre, Environnement, Mécanique (UJF UFR PhiTEM) Université Joseph Fourier - Grenoble 1 (UJF) Accademia Nazionale dei Lincei, ''Centro Beniamino Segre'' Accademia Nazionale dei Lincei, ''Centro Beniamino Segre'', PIIF-GA-2009-236961 PaleoFire 2012-05-03 https://hal-insu.archives-ouvertes.fr/insu-00845304 https://hal-insu.archives-ouvertes.fr/insu-00845304/document https://hal-insu.archives-ouvertes.fr/insu-00845304/file/18196-60949-1-PB.pdf https://doi.org/10.3402/tellusb.v64i0.18196 en eng HAL CCSD Taylor & Francis info:eu-repo/semantics/altIdentifier/doi/10.3402/tellusb.v64i0.18196 insu-00845304 https://hal-insu.archives-ouvertes.fr/insu-00845304 https://hal-insu.archives-ouvertes.fr/insu-00845304/document https://hal-insu.archives-ouvertes.fr/insu-00845304/file/18196-60949-1-PB.pdf doi:10.3402/tellusb.v64i0.18196 info:eu-repo/semantics/OpenAccess ISSN: 0280-6509 EISSN: 1600-0889 Tellus B - Chemical and Physical Meteorology https://hal-insu.archives-ouvertes.fr/insu-00845304 Tellus B - Chemical and Physical Meteorology, 2012, 64, pp.18196. ⟨10.3402/tellusb.v64i0.18196⟩ biomass burning levoglucosan snow ice core Greenland [SDU.STU]Sciences of the Universe [physics]/Earth Sciences info:eu-repo/semantics/article Journal articles 2012 ftunivnantes https://doi.org/10.3402/tellusb.v64i0.18196 2023-02-28T23:59:49Z International audience We demonstrate the use of levoglucosan (1,6-anhydro-β-d-glucopyranose) as a source-specific proxy of past fire activity in snow pits and ice cores. Levoglucosan is unambiguously a degradation product derived from cellulose burning at temperatures greater than 300 °C and is widely used as a biomass burning marker in aerosol analyses. We analyse samples collected from a 3 m snow pit at Summit, Greenland (72°20′N, 38°45′W; 3270 m a.s.l.), with a known depositional history where biomass burning aerosols were traced from their source in a Canadian smoke plume, through their eastward transport and deposition on the Greenland ice sheet, and their eventual burial by accumulating snow layers. The snow pit levoglucosan profile replicates oxalate concentrations from a known forest fire event, suggesting the applicability of levoglucosan as a marker of past fire activity in snow and by extension in ice cores. However, levoglucosan concentration peaks in the snow pit differ from those of ammonium and potassium, which are traditionally used as biomass burning proxies in snow and ice studies but which incorporate sources other than fire activity. The source specificity of levoglucosan can help determine the past relative contribution of biomass burning aerosols when used in conjunction with other proxies in snow and ice. Article in Journal/Newspaper Greenland ice core Ice Sheet Université de Nantes: HAL-UNIV-NANTES Greenland Tellus B: Chemical and Physical Meteorology 64 1 18196