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...
Published in: | Geophysical Research Letters |
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Online Access: | https://hal.science/hal-03103753 https://hal.science/hal-03103753/document https://hal.science/hal-03103753/file/2014GL059561.pdf https://doi.org/10.1002/2014GL059561 |
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ftuniversailles:oai:HAL:hal-03103753v1 2024-04-21T07:46:33+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 Institute for Polar and Marine Research (AWI) Center for Marine Environmental Sciences Bremen (MARUM) Universität Bremen Università degli studi di Trieste = University of Trieste 2014-06-16 https://hal.science/hal-03103753 https://hal.science/hal-03103753/document https://hal.science/hal-03103753/file/2014GL059561.pdf https://doi.org/10.1002/2014GL059561 en eng HAL CCSD American Geophysical Union info:eu-repo/semantics/altIdentifier/doi/10.1002/2014GL059561 hal-03103753 https://hal.science/hal-03103753 https://hal.science/hal-03103753/document https://hal.science/hal-03103753/file/2014GL059561.pdf 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 2024-04-11T00:03:41Z 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 Geophysical Research Letters 41 11 4004 4012 |
institution |
Open Polar |
collection |
Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ |
op_collection_id |
ftuniversailles |
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 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 |
topic_facet |
[SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
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. |
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 Institute for Polar and Marine Research (AWI) Center for Marine Environmental Sciences Bremen (MARUM) Universität Bremen Università degli studi di Trieste = University of Trieste |
format |
Article in Journal/Newspaper |
author |
Pol, K. Masson-Delmotte, Valérie Cattani, O. Debret, Maxime Falourd, S. Jouzel, J. Landais, A. Minster, B. Mudelsee, M. Schulz, M. Stenni, B. |
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. |
title |
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_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_sort |
climate variability features of the last interglacial in the east antarctic epica dome c ice core |
publisher |
HAL CCSD |
publishDate |
2014 |
url |
https://hal.science/hal-03103753 https://hal.science/hal-03103753/document https://hal.science/hal-03103753/file/2014GL059561.pdf https://doi.org/10.1002/2014GL059561 |
genre |
Antarc* Antarctic EPICA ice core |
genre_facet |
Antarc* Antarctic EPICA ice core |
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⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1002/2014GL059561 hal-03103753 https://hal.science/hal-03103753 https://hal.science/hal-03103753/document https://hal.science/hal-03103753/file/2014GL059561.pdf doi:10.1002/2014GL059561 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1002/2014GL059561 |
container_title |
Geophysical Research Letters |
container_volume |
41 |
container_issue |
11 |
container_start_page |
4004 |
op_container_end_page |
4012 |
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1796943947938922496 |