Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling

International audience Although aerosols in the Arctic have multiple and complex impacts on the regional climate, their removal due to deposition is still not well quantified. We combined meteorological , aerosol, precipitation, and snowpack observations with simulations to derive information about...

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Published in:Atmospheric Chemistry and Physics
Main Authors: Jacobi, Hans-Werner, Obleitner, Friedrich, da Costa, Sophie, Ginot, Patrick, Eleftheriadis, Konstantinos, Aas, Wenche, Zanatta, Marco
Other Authors: Institut des Géosciences de l’Environnement (IGE), Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Observatoire des Sciences de l'Univers de Grenoble (OSUG ), 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 Grenoble Alpes 2016-2019 (UGA 2016-2019 ), Institute of Nuclear and Particle Physics (NCSR DEMOKRITOS), Norwegian Institute for Air Research (NILU), Alfred Wegener Institute Potsdam, Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Campus France 31597SM, IPEV 1030, Centre National de la Recherche Scientifique (CNRS) Chantier Arctique Francais/PARCS, German Research Foundation (DFG) 268020496 - TRR 172, ANR-14-AORS-0002,Arctic-ERA,ARCTIC climate change and its impact on Environment, infrastructures and Resource Availability(2014), ANR-10-LABX-0056,OSUG@2020,Innovative strategies for observing and modelling natural systems(2010)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2019
Subjects:
Online Access:https://hal.science/hal-02341811
https://hal.science/hal-02341811/document
https://hal.science/hal-02341811/file/acp-19-10361-2019.pdf
https://doi.org/10.5194/acp-19-10361-2019
id ftunivnantes:oai:HAL:hal-02341811v1
record_format openpolar
institution Open Polar
collection Université de Nantes: HAL-UNIV-NANTES
op_collection_id ftunivnantes
language English
topic [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
spellingShingle [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
Jacobi, Hans-Werner
Obleitner, Friedrich
da Costa, Sophie
Ginot, Patrick
Eleftheriadis, Konstantinos
Aas, Wenche
Zanatta, Marco
Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
topic_facet [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
description International audience Although aerosols in the Arctic have multiple and complex impacts on the regional climate, their removal due to deposition is still not well quantified. We combined meteorological , aerosol, precipitation, and snowpack observations with simulations to derive information about the deposition of sea salt components and black carbon (BC) from Novem-ber 2011 to April 2012 to the Arctic snowpack at two locations close to Ny-Ålesund, Svalbard. The dominating role of sea salt and the contribution of dust for the composition of atmospheric aerosols were reflected in the seasonal composition of the snowpack. The strong alignment of the concentrations of the major sea salt components in the aerosols, the precipitation, and the snowpack is linked to the importance of wet deposition for transfer from the atmosphere to the snow-pack. This agreement was less strong for monthly snow budgets and deposition, indicating important relocation of the impurities inside the snowpack after deposition. Wet deposi-tion was less important for the transfer of nitrate, non-sea-salt sulfate, and BC to the snow during the winter period. The average BC concentration in the snowpack remains small, with a limited impact on snow albedo and melting. Nevertheless, the observations also indicate an important redistribution of BC in the snowpack, leading to layers with enhanced concentrations. The complex behavior of bromide due to modifications during sea salt aerosol formation and remobilization in the atmosphere and in the snow were not resolved because of the lack of bromide measurements in aerosols and precipitation .
author2 Institut des Géosciences de l’Environnement (IGE)
Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Observatoire des Sciences de l'Univers de Grenoble (OSUG )
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 Grenoble Alpes 2016-2019 (UGA 2016-2019 )
Institute of Nuclear and Particle Physics (NCSR DEMOKRITOS)
Norwegian Institute for Air Research (NILU)
Alfred Wegener Institute Potsdam
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI)
Campus France 31597SM
IPEV 1030
Centre National de la Recherche Scientifique (CNRS) Chantier Arctique Francais/PARCS
German Research Foundation (DFG) 268020496 - TRR 172
ANR-14-AORS-0002,Arctic-ERA,ARCTIC climate change and its impact on Environment, infrastructures and Resource Availability(2014)
ANR-10-LABX-0056,OSUG@2020,Innovative strategies for observing and modelling natural systems(2010)
format Article in Journal/Newspaper
author Jacobi, Hans-Werner
Obleitner, Friedrich
da Costa, Sophie
Ginot, Patrick
Eleftheriadis, Konstantinos
Aas, Wenche
Zanatta, Marco
author_facet Jacobi, Hans-Werner
Obleitner, Friedrich
da Costa, Sophie
Ginot, Patrick
Eleftheriadis, Konstantinos
Aas, Wenche
Zanatta, Marco
author_sort Jacobi, Hans-Werner
title Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
title_short Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
title_full Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
title_fullStr Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
title_full_unstemmed Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling
title_sort deposition of ionic species and black carbon to the arctic snowpack: combining snow pit observations with modeling
publisher HAL CCSD
publishDate 2019
url https://hal.science/hal-02341811
https://hal.science/hal-02341811/document
https://hal.science/hal-02341811/file/acp-19-10361-2019.pdf
https://doi.org/10.5194/acp-19-10361-2019
geographic Arctic
Ny-Ålesund
Svalbard
geographic_facet Arctic
Ny-Ålesund
Svalbard
genre albedo
Arctic
black carbon
Ny Ålesund
Ny-Ålesund
Svalbard
genre_facet albedo
Arctic
black carbon
Ny Ålesund
Ny-Ålesund
Svalbard
op_source ISSN: 1680-7316
EISSN: 1680-7324
Atmospheric Chemistry and Physics
https://hal.science/hal-02341811
Atmospheric Chemistry and Physics, 2019, 19 (15), pp.10361-10377. ⟨10.5194/acp-19-10361-2019⟩
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container_title Atmospheric Chemistry and Physics
container_volume 19
container_issue 15
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spelling ftunivnantes:oai:HAL:hal-02341811v1 2023-05-15T13:11:35+02:00 Deposition of ionic species and black carbon to the Arctic snowpack: combining snow pit observations with modeling Jacobi, Hans-Werner Obleitner, Friedrich da Costa, Sophie Ginot, Patrick Eleftheriadis, Konstantinos Aas, Wenche Zanatta, Marco Institut des Géosciences de l’Environnement (IGE) Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Observatoire des Sciences de l'Univers de Grenoble (OSUG ) 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 Grenoble Alpes 2016-2019 (UGA 2016-2019 ) Institute of Nuclear and Particle Physics (NCSR DEMOKRITOS) Norwegian Institute for Air Research (NILU) Alfred Wegener Institute Potsdam Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Campus France 31597SM IPEV 1030 Centre National de la Recherche Scientifique (CNRS) Chantier Arctique Francais/PARCS German Research Foundation (DFG) 268020496 - TRR 172 ANR-14-AORS-0002,Arctic-ERA,ARCTIC climate change and its impact on Environment, infrastructures and Resource Availability(2014) ANR-10-LABX-0056,OSUG@2020,Innovative strategies for observing and modelling natural systems(2010) 2019 https://hal.science/hal-02341811 https://hal.science/hal-02341811/document https://hal.science/hal-02341811/file/acp-19-10361-2019.pdf https://doi.org/10.5194/acp-19-10361-2019 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/acp-19-10361-2019 hal-02341811 https://hal.science/hal-02341811 https://hal.science/hal-02341811/document https://hal.science/hal-02341811/file/acp-19-10361-2019.pdf doi:10.5194/acp-19-10361-2019 WOS: 000481727300001 http://creativecommons.org/licenses/by-nd/ info:eu-repo/semantics/OpenAccess CC-BY-ND ISSN: 1680-7316 EISSN: 1680-7324 Atmospheric Chemistry and Physics https://hal.science/hal-02341811 Atmospheric Chemistry and Physics, 2019, 19 (15), pp.10361-10377. ⟨10.5194/acp-19-10361-2019⟩ [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere info:eu-repo/semantics/article Journal articles 2019 ftunivnantes https://doi.org/10.5194/acp-19-10361-2019 2023-03-01T02:56:36Z International audience Although aerosols in the Arctic have multiple and complex impacts on the regional climate, their removal due to deposition is still not well quantified. We combined meteorological , aerosol, precipitation, and snowpack observations with simulations to derive information about the deposition of sea salt components and black carbon (BC) from Novem-ber 2011 to April 2012 to the Arctic snowpack at two locations close to Ny-Ålesund, Svalbard. The dominating role of sea salt and the contribution of dust for the composition of atmospheric aerosols were reflected in the seasonal composition of the snowpack. The strong alignment of the concentrations of the major sea salt components in the aerosols, the precipitation, and the snowpack is linked to the importance of wet deposition for transfer from the atmosphere to the snow-pack. This agreement was less strong for monthly snow budgets and deposition, indicating important relocation of the impurities inside the snowpack after deposition. Wet deposi-tion was less important for the transfer of nitrate, non-sea-salt sulfate, and BC to the snow during the winter period. The average BC concentration in the snowpack remains small, with a limited impact on snow albedo and melting. Nevertheless, the observations also indicate an important redistribution of BC in the snowpack, leading to layers with enhanced concentrations. The complex behavior of bromide due to modifications during sea salt aerosol formation and remobilization in the atmosphere and in the snow were not resolved because of the lack of bromide measurements in aerosols and precipitation . Article in Journal/Newspaper albedo Arctic black carbon Ny Ålesund Ny-Ålesund Svalbard Université de Nantes: HAL-UNIV-NANTES Arctic Ny-Ålesund Svalbard Atmospheric Chemistry and Physics 19 15 10361 10377