Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core

International audience Whereas millennial to submillennial climate variability has been identified during the current interglacial period, past interglacial variability features remain poorly explored because of lacking data at sufficient temporal resolutions. Here we present new deuterium data from...

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Published in:Geophysical Research Letters
Main Authors: Pol, K., Masson-Delmotte, Valérie, Cattani, O., Debret, Maxime, Falourd, S., Jouzel, J., Landais, A., Minster, B., Mudelsee, M., Schulz, M., Stenni, B.
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA), British Antarctic Survey (BAS), Natural Environment Research Council (NERC), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)), Morphodynamique Continentale et Côtière (M2C), Université de Caen Normandie (UNICAEN), Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN), Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS), Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI), Helmholtz-Gemeinschaft = Helmholtz Association, Center for Marine Environmental Sciences Bremen (MARUM), Universität Bremen Deutschland = University of Bremen Germany = Université de Brême Allemagne, Università degli studi di Trieste = University of Trieste
Format: Article in Journal/Newspaper
Language:English
Published: CCSD 2014
Subjects:
Online Access:https://hal.science/hal-03103753
https://hal.science/hal-03103753v1/document
https://hal.science/hal-03103753v1/file/2014GL059561.pdf
https://doi.org/10.1002/2014GL059561
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author Pol, K.
Masson-Delmotte, Valérie
Cattani, O.
Debret, Maxime
Falourd, S.
Jouzel, J.
Landais, A.
Minster, B.
Mudelsee, M.
Schulz, M.
Stenni, B.
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
British Antarctic Survey (BAS)
Natural Environment Research Council (NERC)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA))
Morphodynamique Continentale et Côtière (M2C)
Université de Caen Normandie (UNICAEN)
Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN)
Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS)
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI)
Helmholtz-Gemeinschaft = Helmholtz Association
Center for Marine Environmental Sciences Bremen (MARUM)
Universität Bremen Deutschland = University of Bremen Germany = Université de Brême Allemagne
Università degli studi di Trieste = University of Trieste
author_facet Pol, K.
Masson-Delmotte, Valérie
Cattani, O.
Debret, Maxime
Falourd, S.
Jouzel, J.
Landais, A.
Minster, B.
Mudelsee, M.
Schulz, M.
Stenni, B.
author_sort Pol, K.
collection Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ
container_issue 11
container_start_page 4004
container_title Geophysical Research Letters
container_volume 41
description International audience Whereas millennial to submillennial climate variability has been identified during the current interglacial period, past interglacial variability features remain poorly explored because of lacking data at sufficient temporal resolutions. Here we present new deuterium data from the EPICA Dome C ice core, documenting at decadal resolution temperature changes occurring over the East Antarctic plateau during the warmer-than-today last interglacial. Expanding previous evidence of instabilities during the last interglacial, multicentennial subevents are identified and labeled for the first time in a past interglacial context. A variance analysis further reveals two major climatic features. First, an increase in variability is detected prior to the glacial inception, as already observed at the end of Marine Isotopic Stage 11 in the same core. Second, the overall variance level is systematically higher during the last interglacial than during the current one, suggesting that a warmer East Antarctic climate may also be more variable.
format Article in Journal/Newspaper
genre Antarc*
Antarctic
EPICA
ice core
genre_facet Antarc*
Antarctic
EPICA
ice core
geographic Antarctic
geographic_facet Antarctic
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institution Open Polar
language English
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op_doi https://doi.org/10.1002/2014GL059561
op_relation info:eu-repo/semantics/altIdentifier/doi/10.1002/2014GL059561
doi:10.1002/2014GL059561
op_rights info:eu-repo/semantics/OpenAccess
op_source ISSN: 0094-8276
EISSN: 1944-8007
Geophysical Research Letters
https://hal.science/hal-03103753
Geophysical Research Letters, 2014, 41 (11), pp.4004-4012. ⟨10.1002/2014GL059561⟩
publishDate 2014
publisher CCSD
record_format openpolar
spelling ftuniversailles:oai:HAL:hal-03103753v1 2025-04-20T14:23:06+00:00 Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core Pol, K. Masson-Delmotte, Valérie Cattani, O. Debret, Maxime Falourd, S. Jouzel, J. Landais, A. Minster, B. Mudelsee, M. Schulz, M. Stenni, B. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) 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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA) British Antarctic Survey (BAS) Natural Environment Research Council (NERC) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-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)-Direction de Recherche Fondamentale (CEA) (DRF (CEA)) Morphodynamique Continentale et Côtière (M2C) Université de Caen Normandie (UNICAEN) Normandie Université (NU)-Normandie Université (NU)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Rouen Normandie (UNIROUEN) Normandie Université (NU)-Centre National de la Recherche Scientifique (CNRS) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association Center for Marine Environmental Sciences Bremen (MARUM) Universität Bremen Deutschland = University of Bremen Germany = Université de Brême Allemagne Università degli studi di Trieste = University of Trieste 2014-06-16 https://hal.science/hal-03103753 https://hal.science/hal-03103753v1/document https://hal.science/hal-03103753v1/file/2014GL059561.pdf https://doi.org/10.1002/2014GL059561 en eng CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2014GL059561 doi:10.1002/2014GL059561 info:eu-repo/semantics/OpenAccess ISSN: 0094-8276 EISSN: 1944-8007 Geophysical Research Letters https://hal.science/hal-03103753 Geophysical Research Letters, 2014, 41 (11), pp.4004-4012. ⟨10.1002/2014GL059561⟩ [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 2014 ftuniversailles https://doi.org/10.1002/2014GL059561 2025-04-09T14:20:41Z International audience Whereas millennial to submillennial climate variability has been identified during the current interglacial period, past interglacial variability features remain poorly explored because of lacking data at sufficient temporal resolutions. Here we present new deuterium data from the EPICA Dome C ice core, documenting at decadal resolution temperature changes occurring over the East Antarctic plateau during the warmer-than-today last interglacial. Expanding previous evidence of instabilities during the last interglacial, multicentennial subevents are identified and labeled for the first time in a past interglacial context. A variance analysis further reveals two major climatic features. First, an increase in variability is detected prior to the glacial inception, as already observed at the end of Marine Isotopic Stage 11 in the same core. Second, the overall variance level is systematically higher during the last interglacial than during the current one, suggesting that a warmer East Antarctic climate may also be more variable. Article in Journal/Newspaper Antarc* Antarctic EPICA ice core Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Antarctic Geophysical Research Letters 41 11 4004 4012
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
Pol, K.
Masson-Delmotte, Valérie
Cattani, O.
Debret, Maxime
Falourd, S.
Jouzel, J.
Landais, A.
Minster, B.
Mudelsee, M.
Schulz, M.
Stenni, B.
Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title_full Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title_fullStr Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title_full_unstemmed Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title_short Climate variability features of the last interglacial in the East Antarctic EPICA Dome C ice core
title_sort climate variability features of the last interglacial in the east antarctic epica dome c ice core
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
url https://hal.science/hal-03103753
https://hal.science/hal-03103753v1/document
https://hal.science/hal-03103753v1/file/2014GL059561.pdf
https://doi.org/10.1002/2014GL059561