Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming
International audience Understanding the role of atmospheric CO$_2$ during past climate changes requires clear knowledge of how it varies in time relative to temperature. Antarctic ice cores preserve highly resolved records of atmospheric CO$_2$ and Antarctic temperature for the past 800,000 years....
Published in: | Science |
---|---|
Main Authors: | , , , , , , , , , |
Other Authors: | , , , , , , , , , , , , , |
Format: | Article in Journal/Newspaper |
Language: | English |
Published: |
HAL CCSD
2013
|
Subjects: | |
Online Access: | https://hal-cea.archives-ouvertes.fr/cea-00862616 https://doi.org/10.1126/science.1226368 |
id |
ftunivnantes:oai:HAL:cea-00862616v1 |
---|---|
record_format |
openpolar |
institution |
Open Polar |
collection |
Université de Nantes: HAL-UNIV-NANTES |
op_collection_id |
ftunivnantes |
language |
English |
topic |
[SDE.MCG]Environmental Sciences/Global Changes [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
spellingShingle |
[SDE.MCG]Environmental Sciences/Global Changes [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology Parrenin, F. Masson-Delmotte, Valérie Köhler, P. Raynaud, D. Paillard, D. Schwander, J. Barbante, C. Landais, Amaelle Wegne, A. Jouzel, Jean Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
topic_facet |
[SDE.MCG]Environmental Sciences/Global Changes [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology |
description |
International audience Understanding the role of atmospheric CO$_2$ during past climate changes requires clear knowledge of how it varies in time relative to temperature. Antarctic ice cores preserve highly resolved records of atmospheric CO$_2$ and Antarctic temperature for the past 800,000 years. Here we propose a revised relative age scale for the concentration of atmospheric CO$_2$ and Antarctic temperature for the last deglacial warming, using data from five Antarctic ice cores. We infer the phasing between CO$_2$ concentration and Antarctic temperature at four times when their trends change abruptly. We find no significant asynchrony between them, indicating that Antarctic temperature did not begin to rise hundreds of years before the concentration of atmospheric CO$_2$, as has been suggested by earlier studies. |
author2 |
Laboratoire de glaciologie et géophysique de l'environnement (LGGE) 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 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)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Modélisation du climat (CLIM) Physics Institute Bern University of Bern Institute for the Dynamics of Environmental Processes-CNR Department of Environmental Sciences Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB) |
format |
Article in Journal/Newspaper |
author |
Parrenin, F. Masson-Delmotte, Valérie Köhler, P. Raynaud, D. Paillard, D. Schwander, J. Barbante, C. Landais, Amaelle Wegne, A. Jouzel, Jean |
author_facet |
Parrenin, F. Masson-Delmotte, Valérie Köhler, P. Raynaud, D. Paillard, D. Schwander, J. Barbante, C. Landais, Amaelle Wegne, A. Jouzel, Jean |
author_sort |
Parrenin, F. |
title |
Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
title_short |
Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
title_full |
Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
title_fullStr |
Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
title_full_unstemmed |
Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming |
title_sort |
synchronous change of atmospheric co$_2$ and antarctic temperature during the last deglacial warming |
publisher |
HAL CCSD |
publishDate |
2013 |
url |
https://hal-cea.archives-ouvertes.fr/cea-00862616 https://doi.org/10.1126/science.1226368 |
geographic |
Antarctic |
geographic_facet |
Antarctic |
genre |
Antarc* Antarctic |
genre_facet |
Antarc* Antarctic |
op_source |
ISSN: 0036-8075 EISSN: 1095-9203 Science https://hal-cea.archives-ouvertes.fr/cea-00862616 Science, 2013, 339 (6130), pp.1060-1063. ⟨10.1126/science.1226368⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1126/science.1226368 cea-00862616 https://hal-cea.archives-ouvertes.fr/cea-00862616 doi:10.1126/science.1226368 |
op_doi |
https://doi.org/10.1126/science.1226368 |
container_title |
Science |
container_volume |
339 |
container_issue |
6123 |
container_start_page |
1060 |
op_container_end_page |
1063 |
_version_ |
1766257069064716288 |
spelling |
ftunivnantes:oai:HAL:cea-00862616v1 2023-05-15T13:52:38+02:00 Synchronous Change of Atmospheric CO$_2$ and Antarctic Temperature During the Last Deglacial Warming Parrenin, F. Masson-Delmotte, Valérie Köhler, P. Raynaud, D. Paillard, D. Schwander, J. Barbante, C. Landais, Amaelle Wegne, A. Jouzel, Jean Laboratoire de glaciologie et géophysique de l'environnement (LGGE) 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 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)-Centre National de la Recherche Scientifique (CNRS) Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung (AWI) Modélisation du climat (CLIM) Physics Institute Bern University of Bern Institute for the Dynamics of Environmental Processes-CNR Department of Environmental Sciences Università degli Studi di Milano-Bicocca = University of Milano-Bicocca (UNIMIB) 2013 https://hal-cea.archives-ouvertes.fr/cea-00862616 https://doi.org/10.1126/science.1226368 en eng HAL CCSD American Association for the Advancement of Science (AAAS) info:eu-repo/semantics/altIdentifier/doi/10.1126/science.1226368 cea-00862616 https://hal-cea.archives-ouvertes.fr/cea-00862616 doi:10.1126/science.1226368 ISSN: 0036-8075 EISSN: 1095-9203 Science https://hal-cea.archives-ouvertes.fr/cea-00862616 Science, 2013, 339 (6130), pp.1060-1063. ⟨10.1126/science.1226368⟩ [SDE.MCG]Environmental Sciences/Global Changes [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2013 ftunivnantes https://doi.org/10.1126/science.1226368 2023-02-28T23:57:25Z International audience Understanding the role of atmospheric CO$_2$ during past climate changes requires clear knowledge of how it varies in time relative to temperature. Antarctic ice cores preserve highly resolved records of atmospheric CO$_2$ and Antarctic temperature for the past 800,000 years. Here we propose a revised relative age scale for the concentration of atmospheric CO$_2$ and Antarctic temperature for the last deglacial warming, using data from five Antarctic ice cores. We infer the phasing between CO$_2$ concentration and Antarctic temperature at four times when their trends change abruptly. We find no significant asynchrony between them, indicating that Antarctic temperature did not begin to rise hundreds of years before the concentration of atmospheric CO$_2$, as has been suggested by earlier studies. Article in Journal/Newspaper Antarc* Antarctic Université de Nantes: HAL-UNIV-NANTES Antarctic Science 339 6123 1060 1063 |