The history of climate dynamics in the late quaternary
International audience Climate variability, defined as changes in integral properties of the atmosphere, is only one small realization of the workings of the much larger earth system. Parts of the other components (ice, ocean, continents) have much slower response times (decadal to millennia). True...
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ftceafr:oai:HAL:hal-02959028v1 2024-06-09T07:47:56+00:00 The history of climate dynamics in the late quaternary Labeyrie, L. Cole, J. Alverson, K. Stocker, T. 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) Paléocéanographie (PALEOCEAN) 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)) Department of Geosciences University of Arizona University of Arizona PAGES International Project Office Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE) 2003 https://hal.science/hal-02959028 https://doi.org/10.1007/978-3-642-55828-3_3 en eng HAL CCSD info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-642-55828-3_3 ISBN: 978-3-642-55828-3 hal-02959028 https://hal.science/hal-02959028 doi:10.1007/978-3-642-55828-3_3 Paleoclimate, Global Change and the Future https://hal.science/hal-02959028 Paleoclimate, Global Change and the Future, pp.33-61, 2003, Global Change - The IGBP Series, 978-3-642-55828-3. ⟨10.1007/978-3-642-55828-3_3⟩ Last Glacial Maximum North Atlantic Oscillation Benthic Foraminifera Thermohaline Circulation North Atlantic Deep Water [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment info:eu-repo/semantics/bookPart Book sections 2003 ftceafr https://doi.org/10.1007/978-3-642-55828-3_3 2024-05-16T14:51:36Z International audience Climate variability, defined as changes in integral properties of the atmosphere, is only one small realization of the workings of the much larger earth system. Parts of the other components (ice, ocean, continents) have much slower response times (decadal to millennia). True understanding of climate dynamics and prediction of future changes will come only with an understanding of the workings of the earth system as a whole, and over both the past and present time scales. Such understanding requires, as a first step, identification of the patterns of climate change on those time scales, and their relationships to known forcing. As a second step, models must be developed to simulate the evolution of the climate system on these same time scales. Within the last few decades, a significant number of long time series have become available that describe paleoclimate variability with resolution better than about 1000 years. Global general circulation models lag however, in that they have yet to be successfully integrated for more than a few hundred years. Book Part North Atlantic Deep Water North Atlantic North Atlantic oscillation HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) 33 61 |
institution |
Open Polar |
collection |
HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) |
op_collection_id |
ftceafr |
language |
English |
topic |
Last Glacial Maximum North Atlantic Oscillation Benthic Foraminifera Thermohaline Circulation North Atlantic Deep Water [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
spellingShingle |
Last Glacial Maximum North Atlantic Oscillation Benthic Foraminifera Thermohaline Circulation North Atlantic Deep Water [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment Labeyrie, L. Cole, J. Alverson, K. Stocker, T. The history of climate dynamics in the late quaternary |
topic_facet |
Last Glacial Maximum North Atlantic Oscillation Benthic Foraminifera Thermohaline Circulation North Atlantic Deep Water [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces environment |
description |
International audience Climate variability, defined as changes in integral properties of the atmosphere, is only one small realization of the workings of the much larger earth system. Parts of the other components (ice, ocean, continents) have much slower response times (decadal to millennia). True understanding of climate dynamics and prediction of future changes will come only with an understanding of the workings of the earth system as a whole, and over both the past and present time scales. Such understanding requires, as a first step, identification of the patterns of climate change on those time scales, and their relationships to known forcing. As a second step, models must be developed to simulate the evolution of the climate system on these same time scales. Within the last few decades, a significant number of long time series have become available that describe paleoclimate variability with resolution better than about 1000 years. Global general circulation models lag however, in that they have yet to be successfully integrated for more than a few hundred years. |
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) Paléocéanographie (PALEOCEAN) 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)) Department of Geosciences University of Arizona University of Arizona PAGES International Project Office Climate and Environmental Physics Bern (CEP) Physikalisches Institut Bern Universität Bern / University of Bern (UNIBE)-Universität Bern / University of Bern (UNIBE) |
format |
Book Part |
author |
Labeyrie, L. Cole, J. Alverson, K. Stocker, T. |
author_facet |
Labeyrie, L. Cole, J. Alverson, K. Stocker, T. |
author_sort |
Labeyrie, L. |
title |
The history of climate dynamics in the late quaternary |
title_short |
The history of climate dynamics in the late quaternary |
title_full |
The history of climate dynamics in the late quaternary |
title_fullStr |
The history of climate dynamics in the late quaternary |
title_full_unstemmed |
The history of climate dynamics in the late quaternary |
title_sort |
history of climate dynamics in the late quaternary |
publisher |
HAL CCSD |
publishDate |
2003 |
url |
https://hal.science/hal-02959028 https://doi.org/10.1007/978-3-642-55828-3_3 |
genre |
North Atlantic Deep Water North Atlantic North Atlantic oscillation |
genre_facet |
North Atlantic Deep Water North Atlantic North Atlantic oscillation |
op_source |
Paleoclimate, Global Change and the Future https://hal.science/hal-02959028 Paleoclimate, Global Change and the Future, pp.33-61, 2003, Global Change - The IGBP Series, 978-3-642-55828-3. ⟨10.1007/978-3-642-55828-3_3⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1007/978-3-642-55828-3_3 ISBN: 978-3-642-55828-3 hal-02959028 https://hal.science/hal-02959028 doi:10.1007/978-3-642-55828-3_3 |
op_doi |
https://doi.org/10.1007/978-3-642-55828-3_3 |
container_start_page |
33 |
op_container_end_page |
61 |
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1801379421320380416 |