Water Isotopic Signature of Surface Snow Metamorphism in Antarctica

International audience In low accumulation regions of Antarctica, precipitation is so sparse that the processes occurring after snowfall (post-deposition), such as surface metamorphism (Picard et al., 2012), sublimation and solid condensation (Genthon et al., 2017), as well as the redistribution of...

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Published in:Geophysical Research Letters
Main Authors: Casado, Mathieu, Landais, Amaelle, Picard, Ghislain, Arnaud, Laurent, Dreossi, Giuliano, Stenni, Barbara, Prié, Frederic
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI), Institute of Environmental Physics Heidelberg (IUP), Universität Heidelberg Heidelberg, Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Institut des Géosciences de l’Environnement (IGE), Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ), Université Grenoble Alpes (UGA), Institute of Polar Sciences Venezia-Mestre (CNR-ISP), Consiglio Nazionale delle Ricerche Roma (CNR), Dipartimento di Scienze Ambientali, Informatica e Statistica Venezia (DAIS), University of Ca’ Foscari Venice, Italy
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2021
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-03348483
https://hal.archives-ouvertes.fr/hal-03348483/document
https://hal.archives-ouvertes.fr/hal-03348483/file/2021GL093382.pdf
https://doi.org/10.1029/2021gl093382
id ftccsdartic:oai:HAL:hal-03348483v1
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.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Casado, Mathieu
Landais, Amaelle
Picard, Ghislain
Arnaud, Laurent
Dreossi, Giuliano
Stenni, Barbara
Prié, Frederic
Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience In low accumulation regions of Antarctica, precipitation is so sparse that the processes occurring after snowfall (post-deposition), such as surface metamorphism (Picard et al., 2012), sublimation and solid condensation (Genthon et al., 2017), as well as the redistribution of snow by wind (Groot Zwaaftink et al., 2013; Picard et al., 2019), play a prominent role in how snow accumulates to build the snowpack. These processes strongly affect the physical properties (albedo, density, and grain size) and geochemical composition of snow. For instance, snow grain size, which controls the albedo (Grenfell et al., 1994; Wiscombe & Warren, 1980), is the result of the competition between precipitation which brings small size grains on the surface and metamorphism which coarsens existing grains (Picard et al., 2012). These post-deposition processes influence the snow isotopic composition (δ 18 O or δD for the first order) that are traditionally interpreted as proxies of past temperatures in ice cores. Before deposition, the link between temperature and δ 18 O is due to the Rayleigh distillation of moist air from evaporation sites at low latitudes to the high-latitude precipitation sites (Dansgaard, 1964): When temperature decreases and precipitation occurs, the condensed phase becomes enriched and the remaining moisture depleted of heavy isotopes. In Antarctica, ice cores covering several glacial-interglacial transitions have been retrieved from sites that combine two assets: large ice thickness and low accumulation (EPICA, 2004; Kawamura et al., 2017; Petit et al., 1999). However, the low accumulation lead to the contributions from poorly
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI)
Institute of Environmental Physics Heidelberg (IUP)
Universität Heidelberg Heidelberg
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Institut des Géosciences de l’Environnement (IGE)
Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP )
Université Grenoble Alpes (UGA)
Institute of Polar Sciences Venezia-Mestre (CNR-ISP)
Consiglio Nazionale delle Ricerche Roma (CNR)
Dipartimento di Scienze Ambientali, Informatica e Statistica Venezia (DAIS)
University of Ca’ Foscari Venice, Italy
format Article in Journal/Newspaper
author Casado, Mathieu
Landais, Amaelle
Picard, Ghislain
Arnaud, Laurent
Dreossi, Giuliano
Stenni, Barbara
Prié, Frederic
author_facet Casado, Mathieu
Landais, Amaelle
Picard, Ghislain
Arnaud, Laurent
Dreossi, Giuliano
Stenni, Barbara
Prié, Frederic
author_sort Casado, Mathieu
title Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
title_short Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
title_full Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
title_fullStr Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
title_full_unstemmed Water Isotopic Signature of Surface Snow Metamorphism in Antarctica
title_sort water isotopic signature of surface snow metamorphism in antarctica
publisher HAL CCSD
publishDate 2021
url https://hal.archives-ouvertes.fr/hal-03348483
https://hal.archives-ouvertes.fr/hal-03348483/document
https://hal.archives-ouvertes.fr/hal-03348483/file/2021GL093382.pdf
https://doi.org/10.1029/2021gl093382
genre Antarc*
Antarctica
EPICA
genre_facet Antarc*
Antarctica
EPICA
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.archives-ouvertes.fr/hal-03348483
Geophysical Research Letters, American Geophysical Union, 2021, 48 (17), ⟨10.1029/2021gl093382⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1029/2021gl093382
hal-03348483
https://hal.archives-ouvertes.fr/hal-03348483
https://hal.archives-ouvertes.fr/hal-03348483/document
https://hal.archives-ouvertes.fr/hal-03348483/file/2021GL093382.pdf
doi:10.1029/2021gl093382
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.1029/2021gl093382
container_title Geophysical Research Letters
container_volume 48
container_issue 17
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spelling ftccsdartic:oai:HAL:hal-03348483v1 2023-05-15T13:49:06+02:00 Water Isotopic Signature of Surface Snow Metamorphism in Antarctica Casado, Mathieu Landais, Amaelle Picard, Ghislain Arnaud, Laurent Dreossi, Giuliano Stenni, Barbara Prié, Frederic Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Institute of Environmental Physics Heidelberg (IUP) Universität Heidelberg Heidelberg Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Institut des Géosciences de l’Environnement (IGE) Université Grenoble Alpes (UGA)-Centre National de la Recherche Scientifique (CNRS)-Institut national des sciences de l'Univers (INSU - CNRS)-Institut de Recherche pour le Développement (IRD)-Institut polytechnique de Grenoble - Grenoble Institute of Technology (Grenoble INP ) Université Grenoble Alpes (UGA) Institute of Polar Sciences Venezia-Mestre (CNR-ISP) Consiglio Nazionale delle Ricerche Roma (CNR) Dipartimento di Scienze Ambientali, Informatica e Statistica Venezia (DAIS) University of Ca’ Foscari Venice, Italy 2021-09-03 https://hal.archives-ouvertes.fr/hal-03348483 https://hal.archives-ouvertes.fr/hal-03348483/document https://hal.archives-ouvertes.fr/hal-03348483/file/2021GL093382.pdf https://doi.org/10.1029/2021gl093382 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1029/2021gl093382 hal-03348483 https://hal.archives-ouvertes.fr/hal-03348483 https://hal.archives-ouvertes.fr/hal-03348483/document https://hal.archives-ouvertes.fr/hal-03348483/file/2021GL093382.pdf doi:10.1029/2021gl093382 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.archives-ouvertes.fr/hal-03348483 Geophysical Research Letters, American Geophysical Union, 2021, 48 (17), ⟨10.1029/2021gl093382⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/article Journal articles 2021 ftccsdartic https://doi.org/10.1029/2021gl093382 2022-01-09T00:10:50Z International audience In low accumulation regions of Antarctica, precipitation is so sparse that the processes occurring after snowfall (post-deposition), such as surface metamorphism (Picard et al., 2012), sublimation and solid condensation (Genthon et al., 2017), as well as the redistribution of snow by wind (Groot Zwaaftink et al., 2013; Picard et al., 2019), play a prominent role in how snow accumulates to build the snowpack. These processes strongly affect the physical properties (albedo, density, and grain size) and geochemical composition of snow. For instance, snow grain size, which controls the albedo (Grenfell et al., 1994; Wiscombe & Warren, 1980), is the result of the competition between precipitation which brings small size grains on the surface and metamorphism which coarsens existing grains (Picard et al., 2012). These post-deposition processes influence the snow isotopic composition (δ 18 O or δD for the first order) that are traditionally interpreted as proxies of past temperatures in ice cores. Before deposition, the link between temperature and δ 18 O is due to the Rayleigh distillation of moist air from evaporation sites at low latitudes to the high-latitude precipitation sites (Dansgaard, 1964): When temperature decreases and precipitation occurs, the condensed phase becomes enriched and the remaining moisture depleted of heavy isotopes. In Antarctica, ice cores covering several glacial-interglacial transitions have been retrieved from sites that combine two assets: large ice thickness and low accumulation (EPICA, 2004; Kawamura et al., 2017; Petit et al., 1999). However, the low accumulation lead to the contributions from poorly Article in Journal/Newspaper Antarc* Antarctica EPICA Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Geophysical Research Letters 48 17