Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime

International audience A field campaign was conducted in Ny-Ǻlesund (78°54'N, 11°53'E), Svalbard (Norway) during April and May 2005. An Atmospheric Mercury (Hg) Depletion Event (AMDE) was observed from the morning of April 24 until the evening of April 27. Transport of already Hg and ozone...

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Published in:Science of The Total Environment
Main Authors: P. Ferrari, Christophe, Padova, Cyril, Faïn, Xavier, Gauchard, Pierre-Alexis, Dommergue, Aurélien, Aspmo, Katrine, Berg, Torunn, Cairns, Warren, Barbante, Carlo, Cescon, Paolo, Kaleschke, Lars, Richter, Andreas, Wittrock, Folkard, Boutron, Claude
Other Authors: Laboratoire de glaciologie et géophysique de l'environnement (LGGE), Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-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 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), Polytech' Grenoble, Université Joseph Fourier - Grenoble 1 (UJF), Norwegian Institute for Air Research (NILU), Department of Chemistry Oslo, Faculty of Mathematics and Natural Sciences Oslo, University of Oslo (UiO)-University of Oslo (UiO), Institute for the Dynamics of Environmental Processes-CNR, University of Ca’ Foscari Venice, Italy, Environmental Sciences Department, Institute of Oceanography Hamburg, University of Hamburg, Institute of Environmental Physics Bremen (IUP), University of Bremen, Unité de Formation et de Recherche de Physique
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2008
Subjects:
Online Access:https://hal-insu.archives-ouvertes.fr/insu-00378389
https://doi.org/10.1016/j.scitotenv.2008.01.064
id ftccsdartic:oai:HAL:insu-00378389v1
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 Mercury
Snow
Deposition
Chemical transformation
AMDEs
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle Mercury
Snow
Deposition
Chemical transformation
AMDEs
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
P. Ferrari, Christophe
Padova, Cyril
Faïn, Xavier
Gauchard, Pierre-Alexis
Dommergue, Aurélien
Aspmo, Katrine
Berg, Torunn
Cairns, Warren,
Barbante, Carlo
Cescon, Paolo
Kaleschke, Lars
Richter, Andreas
Wittrock, Folkard
Boutron, Claude
Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
topic_facet Mercury
Snow
Deposition
Chemical transformation
AMDEs
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience A field campaign was conducted in Ny-Ǻlesund (78°54'N, 11°53'E), Svalbard (Norway) during April and May 2005. An Atmospheric Mercury (Hg) Depletion Event (AMDE) was observed from the morning of April 24 until the evening of April 27. Transport of already Hg and ozone (O3) depleted air masses could explain this observed depletion. Due to a snowfall event during the AMDE, surface snow Hg concentrations increased two fold. Hg deposition took place over a short period of time corresponding to 3–4 days. More than 80% of the deposited Hg was estimated to be reemitted back to the atmosphere in the days following the event. During the campaign, we observed night and day variations in surface snow Hg concentrations, which may be the result of gaseous elemental mercury (GEM) oxidation to divalent Hg at the snow/air interface by daylight surface snow chemistry. Finally, a decrease in the reactive Hg (HgR) fraction of total Hg (HgT) in the surface snow was observed during spring. We postulate that the transformation of HgR to a more stable form may occur in Arctic snow during spring.
author2 Laboratoire de glaciologie et géophysique de l'environnement (LGGE)
Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-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 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)
Polytech' Grenoble
Université Joseph Fourier - Grenoble 1 (UJF)
Norwegian Institute for Air Research (NILU)
Department of Chemistry Oslo
Faculty of Mathematics and Natural Sciences Oslo
University of Oslo (UiO)-University of Oslo (UiO)
Institute for the Dynamics of Environmental Processes-CNR
University of Ca’ Foscari Venice, Italy
Environmental Sciences Department
Institute of Oceanography Hamburg
University of Hamburg
Institute of Environmental Physics Bremen (IUP)
University of Bremen
Unité de Formation et de Recherche de Physique
format Article in Journal/Newspaper
author P. Ferrari, Christophe
Padova, Cyril
Faïn, Xavier
Gauchard, Pierre-Alexis
Dommergue, Aurélien
Aspmo, Katrine
Berg, Torunn
Cairns, Warren,
Barbante, Carlo
Cescon, Paolo
Kaleschke, Lars
Richter, Andreas
Wittrock, Folkard
Boutron, Claude
author_facet P. Ferrari, Christophe
Padova, Cyril
Faïn, Xavier
Gauchard, Pierre-Alexis
Dommergue, Aurélien
Aspmo, Katrine
Berg, Torunn
Cairns, Warren,
Barbante, Carlo
Cescon, Paolo
Kaleschke, Lars
Richter, Andreas
Wittrock, Folkard
Boutron, Claude
author_sort P. Ferrari, Christophe
title Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
title_short Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
title_full Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
title_fullStr Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
title_full_unstemmed Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime
title_sort atmospheric mercury depletion event study in ny-alesund (svalbard) in spring 2005. deposition and transformation of hg in surface snow during springtime
publisher HAL CCSD
publishDate 2008
url https://hal-insu.archives-ouvertes.fr/insu-00378389
https://doi.org/10.1016/j.scitotenv.2008.01.064
geographic Arctic
Norway
Svalbard
geographic_facet Arctic
Norway
Svalbard
genre Arctic
Svalbard
genre_facet Arctic
Svalbard
op_source ISSN: 0048-9697
EISSN: 1879-1026
Science of the Total Environment
https://hal-insu.archives-ouvertes.fr/insu-00378389
Science of the Total Environment, Elsevier, 2008, 397 (1-3), pp.167 à 177. ⟨10.1016/j.scitotenv.2008.01.064⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1016/j.scitotenv.2008.01.064
insu-00378389
https://hal-insu.archives-ouvertes.fr/insu-00378389
doi:10.1016/j.scitotenv.2008.01.064
op_doi https://doi.org/10.1016/j.scitotenv.2008.01.064
container_title Science of The Total Environment
container_volume 397
container_issue 1-3
container_start_page 167
op_container_end_page 177
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spelling ftccsdartic:oai:HAL:insu-00378389v1 2023-05-15T15:07:31+02:00 Atmospheric mercury depletion event study in Ny-Alesund (Svalbard) in spring 2005. Deposition and transformation of Hg in surface snow during springtime P. Ferrari, Christophe Padova, Cyril Faïn, Xavier Gauchard, Pierre-Alexis Dommergue, Aurélien Aspmo, Katrine Berg, Torunn Cairns, Warren, Barbante, Carlo Cescon, Paolo Kaleschke, Lars Richter, Andreas Wittrock, Folkard Boutron, Claude Laboratoire de glaciologie et géophysique de l'environnement (LGGE) Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-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 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) Polytech' Grenoble Université Joseph Fourier - Grenoble 1 (UJF) Norwegian Institute for Air Research (NILU) Department of Chemistry Oslo Faculty of Mathematics and Natural Sciences Oslo University of Oslo (UiO)-University of Oslo (UiO) Institute for the Dynamics of Environmental Processes-CNR University of Ca’ Foscari Venice, Italy Environmental Sciences Department Institute of Oceanography Hamburg University of Hamburg Institute of Environmental Physics Bremen (IUP) University of Bremen Unité de Formation et de Recherche de Physique 2008 https://hal-insu.archives-ouvertes.fr/insu-00378389 https://doi.org/10.1016/j.scitotenv.2008.01.064 en eng HAL CCSD Elsevier info:eu-repo/semantics/altIdentifier/doi/10.1016/j.scitotenv.2008.01.064 insu-00378389 https://hal-insu.archives-ouvertes.fr/insu-00378389 doi:10.1016/j.scitotenv.2008.01.064 ISSN: 0048-9697 EISSN: 1879-1026 Science of the Total Environment https://hal-insu.archives-ouvertes.fr/insu-00378389 Science of the Total Environment, Elsevier, 2008, 397 (1-3), pp.167 à 177. ⟨10.1016/j.scitotenv.2008.01.064⟩ Mercury Snow Deposition Chemical transformation AMDEs [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 2008 ftccsdartic https://doi.org/10.1016/j.scitotenv.2008.01.064 2021-10-24T20:05:13Z International audience A field campaign was conducted in Ny-Ǻlesund (78°54'N, 11°53'E), Svalbard (Norway) during April and May 2005. An Atmospheric Mercury (Hg) Depletion Event (AMDE) was observed from the morning of April 24 until the evening of April 27. Transport of already Hg and ozone (O3) depleted air masses could explain this observed depletion. Due to a snowfall event during the AMDE, surface snow Hg concentrations increased two fold. Hg deposition took place over a short period of time corresponding to 3–4 days. More than 80% of the deposited Hg was estimated to be reemitted back to the atmosphere in the days following the event. During the campaign, we observed night and day variations in surface snow Hg concentrations, which may be the result of gaseous elemental mercury (GEM) oxidation to divalent Hg at the snow/air interface by daylight surface snow chemistry. Finally, a decrease in the reactive Hg (HgR) fraction of total Hg (HgT) in the surface snow was observed during spring. We postulate that the transformation of HgR to a more stable form may occur in Arctic snow during spring. Article in Journal/Newspaper Arctic Svalbard Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Norway Svalbard Science of The Total Environment 397 1-3 167 177