Evidence for general instability of past climate from a 250-kyr ice-core record

International audience RECENT results from two ice cores drilled in central Greenland have revealed large, abrupt climate changes of at least regional extent during the late stages of the last glaciation, suggesting that climate in the North Atlantic region is able to reorganize itself rapidly, perh...

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Published in:Nature
Main Authors: Dansgaard, W., Johnsen, S. J., Clausen, H. B., Dahl-Jensen, D., Gundestrup, N. S., Hammer, C. U., Hvidberg, C. S., Steffensen, J. P., Sveinbjörnsdottir, A. E., Jouzel, Jean, Bond, G.
Other Authors: Centre for Ice and Climate Copenhagen, Niels Bohr Institute Copenhagen (NBI), Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen, University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH), University of Iceland Reykjavik, 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), CEA / DSM, Commissariat à l'énergie atomique et aux énergies alternatives (CEA), Lamont-Doherty Earth Observatory (LDEO), Columbia University New York
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 1993
Subjects:
Online Access:https://hal.science/hal-01103728
https://hal.science/hal-01103728/document
https://hal.science/hal-01103728/file/Dansgaard1993.pdf
https://doi.org/10.1038/364218a0
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institution Open Polar
collection Institut national des sciences de l'Univers: HAL-INSU
op_collection_id ftinsu
language English
topic [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
spellingShingle [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
Dansgaard, W.
Johnsen, S. J.
Clausen, H. B.
Dahl-Jensen, D.
Gundestrup, N. S.
Hammer, C. U.
Hvidberg, C. S.
Steffensen, J. P.
Sveinbjörnsdottir, A. E.
Jouzel, Jean
Bond, G.
Evidence for general instability of past climate from a 250-kyr ice-core record
topic_facet [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
[SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology
description International audience RECENT results from two ice cores drilled in central Greenland have revealed large, abrupt climate changes of at least regional extent during the late stages of the last glaciation, suggesting that climate in the North Atlantic region is able to reorganize itself rapidly, perhaps even within a few decades. Here we present a detailed stable-isotope record for the full length of the Greenland Ice-core Project Summit ice core, extending over the past 250 kyr according to a calculated timescale. We find that climate instability was not confined to the last glaciation, but appears also to have been marked during the last interglacial (as explored more fully in a companion paper) and during the previous Saale–Holstein glacial cycle. This is in contrast with the extreme stability of the Holocene, suggesting that recent climate stability may be the exception rather than the rule. The last interglacial seems to have lasted longer than is implied by the deep-sea SPECMAP record, in agreement with other land-based observations. We suggest that climate instability in the early part of the last interglacial may have delayed the melting of the Saalean ice sheets in America and Eurasia, perhaps accounting for this discrepancy.
author2 Centre for Ice and Climate Copenhagen
Niels Bohr Institute Copenhagen (NBI)
Faculty of Science Copenhagen
University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen
University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)
University of Iceland Reykjavik
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)
CEA / DSM
Commissariat à l'énergie atomique et aux énergies alternatives (CEA)
Lamont-Doherty Earth Observatory (LDEO)
Columbia University New York
format Article in Journal/Newspaper
author Dansgaard, W.
Johnsen, S. J.
Clausen, H. B.
Dahl-Jensen, D.
Gundestrup, N. S.
Hammer, C. U.
Hvidberg, C. S.
Steffensen, J. P.
Sveinbjörnsdottir, A. E.
Jouzel, Jean
Bond, G.
author_facet Dansgaard, W.
Johnsen, S. J.
Clausen, H. B.
Dahl-Jensen, D.
Gundestrup, N. S.
Hammer, C. U.
Hvidberg, C. S.
Steffensen, J. P.
Sveinbjörnsdottir, A. E.
Jouzel, Jean
Bond, G.
author_sort Dansgaard, W.
title Evidence for general instability of past climate from a 250-kyr ice-core record
title_short Evidence for general instability of past climate from a 250-kyr ice-core record
title_full Evidence for general instability of past climate from a 250-kyr ice-core record
title_fullStr Evidence for general instability of past climate from a 250-kyr ice-core record
title_full_unstemmed Evidence for general instability of past climate from a 250-kyr ice-core record
title_sort evidence for general instability of past climate from a 250-kyr ice-core record
publisher HAL CCSD
publishDate 1993
url https://hal.science/hal-01103728
https://hal.science/hal-01103728/document
https://hal.science/hal-01103728/file/Dansgaard1993.pdf
https://doi.org/10.1038/364218a0
genre Greenland
Greenland ice core
Greenland Ice core Project
ice core
North Atlantic
genre_facet Greenland
Greenland ice core
Greenland Ice core Project
ice core
North Atlantic
op_source ISSN: 0028-0836
EISSN: 1476-4687
Nature
https://hal.science/hal-01103728
Nature, 1993, 364 (6434), pp.218-220. ⟨10.1038/364218a0⟩
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https://hal.science/hal-01103728/document
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container_title Nature
container_volume 364
container_issue 6434
container_start_page 218
op_container_end_page 220
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spelling ftinsu:oai:HAL:hal-01103728v1 2024-04-28T08:21:28+00:00 Evidence for general instability of past climate from a 250-kyr ice-core record Dansgaard, W. Johnsen, S. J. Clausen, H. B. Dahl-Jensen, D. Gundestrup, N. S. Hammer, C. U. Hvidberg, C. S. Steffensen, J. P. Sveinbjörnsdottir, A. E. Jouzel, Jean Bond, G. Centre for Ice and Climate Copenhagen Niels Bohr Institute Copenhagen (NBI) Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH)-Faculty of Science Copenhagen University of Copenhagen = Københavns Universitet (UCPH)-University of Copenhagen = Københavns Universitet (UCPH) University of Iceland Reykjavik 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) CEA / DSM Commissariat à l'énergie atomique et aux énergies alternatives (CEA) Lamont-Doherty Earth Observatory (LDEO) Columbia University New York 1993 https://hal.science/hal-01103728 https://hal.science/hal-01103728/document https://hal.science/hal-01103728/file/Dansgaard1993.pdf https://doi.org/10.1038/364218a0 en eng HAL CCSD Nature Publishing Group info:eu-repo/semantics/altIdentifier/doi/10.1038/364218a0 hal-01103728 https://hal.science/hal-01103728 https://hal.science/hal-01103728/document https://hal.science/hal-01103728/file/Dansgaard1993.pdf doi:10.1038/364218a0 http://creativecommons.org/licenses/by-nc/ info:eu-repo/semantics/OpenAccess ISSN: 0028-0836 EISSN: 1476-4687 Nature https://hal.science/hal-01103728 Nature, 1993, 364 (6434), pp.218-220. ⟨10.1038/364218a0⟩ [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.GL]Sciences of the Universe [physics]/Earth Sciences/Glaciology info:eu-repo/semantics/article Journal articles 1993 ftinsu https://doi.org/10.1038/364218a0 2024-04-05T00:31:43Z International audience RECENT results from two ice cores drilled in central Greenland have revealed large, abrupt climate changes of at least regional extent during the late stages of the last glaciation, suggesting that climate in the North Atlantic region is able to reorganize itself rapidly, perhaps even within a few decades. Here we present a detailed stable-isotope record for the full length of the Greenland Ice-core Project Summit ice core, extending over the past 250 kyr according to a calculated timescale. We find that climate instability was not confined to the last glaciation, but appears also to have been marked during the last interglacial (as explored more fully in a companion paper) and during the previous Saale–Holstein glacial cycle. This is in contrast with the extreme stability of the Holocene, suggesting that recent climate stability may be the exception rather than the rule. The last interglacial seems to have lasted longer than is implied by the deep-sea SPECMAP record, in agreement with other land-based observations. We suggest that climate instability in the early part of the last interglacial may have delayed the melting of the Saalean ice sheets in America and Eurasia, perhaps accounting for this discrepancy. Article in Journal/Newspaper Greenland Greenland ice core Greenland Ice core Project ice core North Atlantic Institut national des sciences de l'Univers: HAL-INSU Nature 364 6434 218 220