Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments

International audience We describe the creation of a data set describing changes related to the presence of ice sheets, including ice-sheet extent and height, ice-shelf extent, and the distribution and elevation of ice-free land at the Last Glacial Maximum (LGM), which were used in LGM experiments c...

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Published in:Geoscientific Model Development
Main Authors: Abe-Ouchi, A., Saito, F., Kageyama, M., Braconnot, P., Harrison, S., Lambeck, K., Otto-Bliesner, L., Peltier, W., Tarasov, L., Peterschmitt, J.-Y., Takahashi, K.
Other Authors: Center for Climate System Research Kashiwa (CCSR), The University of Tokyo (UTokyo), 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), Modélisation du climat (CLIM), 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)), Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID), Department of Physics and Physical Oceanography, Memorial University of Newfoundland = Université Memorial de Terre-Neuve St. John's, Canada (MUN), Institute of Research and Innovation, Japan
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
Online Access:https://hal.science/hal-01805253
https://hal.science/hal-01805253/document
https://hal.science/hal-01805253/file/gmd-8-3621-2015.pdf
https://doi.org/10.5194/gmd-8-3621-2015
id ftuniversailles:oai:HAL:hal-01805253v1
record_format openpolar
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
Abe-Ouchi, A.
Saito, F.
Kageyama, M.
Braconnot, P.
Harrison, S.
Lambeck, K.
Otto-Bliesner, L.
Peltier, W.
Tarasov, L.
Peterschmitt, J.-Y.
Takahashi, K.
Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience We describe the creation of a data set describing changes related to the presence of ice sheets, including ice-sheet extent and height, ice-shelf extent, and the distribution and elevation of ice-free land at the Last Glacial Maximum (LGM), which were used in LGM experiments conducted as part of the fifth phase of the Coupled Modelling Intercomparison Project (CMIP5) and the third phase of the Palaeoclimate Modelling Intercomparison Project (PMIP3). The CMIP5/PMIP3 data sets were created from reconstructions made by three different groups, which were all obtained using a model-inversion approach but differ in the assumptions used in the modelling and in the type of data used as constraints. The ice-sheet extent in the Northern Hemisphere (NH) does not vary substantially between the three individual data sources. The difference in the topography of the NH ice sheets is also moderate, and smaller than the differences between these reconstructions (and the resultant composite reconstruction) and ice-sheet reconstructions used in previous generations of PMIP. Only two of the individual reconstructions provide information for Antarctica. The discrepancy between these two reconstructions is larger than the difference for the NH ice sheets, although still less than the difference between the composite reconstruction and previous PMIP ice-sheet reconstructions. Although largely confined to the ice-covered regions, differences between the climate response to the individual LGM reconstructions extend over the North Atlantic Ocean and Northern Hemisphere continents , partly through atmospheric stationary waves. Differences between the climate response to the CMIP5/PMIP3 composite and any individual ice-sheet reconstruction are smaller than those between the CMIP5/PMIP3 composite and the ice sheet used in the last phase of PMIP (PMIP2).
author2 Center for Climate System Research Kashiwa (CCSR)
The University of Tokyo (UTokyo)
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)
Modélisation du climat (CLIM)
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))
Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID)
Department of Physics and Physical Oceanography
Memorial University of Newfoundland = Université Memorial de Terre-Neuve St. John's, Canada (MUN)
Institute of Research and Innovation, Japan
format Article in Journal/Newspaper
author Abe-Ouchi, A.
Saito, F.
Kageyama, M.
Braconnot, P.
Harrison, S.
Lambeck, K.
Otto-Bliesner, L.
Peltier, W.
Tarasov, L.
Peterschmitt, J.-Y.
Takahashi, K.
author_facet Abe-Ouchi, A.
Saito, F.
Kageyama, M.
Braconnot, P.
Harrison, S.
Lambeck, K.
Otto-Bliesner, L.
Peltier, W.
Tarasov, L.
Peterschmitt, J.-Y.
Takahashi, K.
author_sort Abe-Ouchi, A.
title Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
title_short Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
title_full Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
title_fullStr Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
title_full_unstemmed Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments
title_sort ice-sheet configuration in the cmip5/pmip3 last glacial maximum experiments
publisher HAL CCSD
publishDate 2015
url https://hal.science/hal-01805253
https://hal.science/hal-01805253/document
https://hal.science/hal-01805253/file/gmd-8-3621-2015.pdf
https://doi.org/10.5194/gmd-8-3621-2015
genre Antarc*
Antarctica
Ice Sheet
Ice Shelf
North Atlantic
genre_facet Antarc*
Antarctica
Ice Sheet
Ice Shelf
North Atlantic
op_source ISSN: 1991-9603
EISSN: 1991-959X
Geoscientific Model Development
https://hal.science/hal-01805253
Geoscientific Model Development, 2015, 8 (11), pp.3621 - 3637. ⟨10.5194/gmd-8-3621-2015⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/gmd-8-3621-2015
hal-01805253
https://hal.science/hal-01805253
https://hal.science/hal-01805253/document
https://hal.science/hal-01805253/file/gmd-8-3621-2015.pdf
doi:10.5194/gmd-8-3621-2015
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/gmd-8-3621-2015
container_title Geoscientific Model Development
container_volume 8
container_issue 11
container_start_page 3621
op_container_end_page 3637
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spelling ftuniversailles:oai:HAL:hal-01805253v1 2024-04-28T08:01:48+00:00 Ice-sheet configuration in the CMIP5/PMIP3 Last Glacial Maximum experiments Abe-Ouchi, A. Saito, F. Kageyama, M. Braconnot, P. Harrison, S. Lambeck, K. Otto-Bliesner, L. Peltier, W. Tarasov, L. Peterschmitt, J.-Y. Takahashi, K. Center for Climate System Research Kashiwa (CCSR) The University of Tokyo (UTokyo) 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) Modélisation du climat (CLIM) 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)) Modelling the Earth Response to Multiple Anthropogenic Interactions and Dynamics (MERMAID) Department of Physics and Physical Oceanography Memorial University of Newfoundland = Université Memorial de Terre-Neuve St. John's, Canada (MUN) Institute of Research and Innovation, Japan 2015 https://hal.science/hal-01805253 https://hal.science/hal-01805253/document https://hal.science/hal-01805253/file/gmd-8-3621-2015.pdf https://doi.org/10.5194/gmd-8-3621-2015 en eng HAL CCSD European Geosciences Union info:eu-repo/semantics/altIdentifier/doi/10.5194/gmd-8-3621-2015 hal-01805253 https://hal.science/hal-01805253 https://hal.science/hal-01805253/document https://hal.science/hal-01805253/file/gmd-8-3621-2015.pdf doi:10.5194/gmd-8-3621-2015 info:eu-repo/semantics/OpenAccess ISSN: 1991-9603 EISSN: 1991-959X Geoscientific Model Development https://hal.science/hal-01805253 Geoscientific Model Development, 2015, 8 (11), pp.3621 - 3637. ⟨10.5194/gmd-8-3621-2015⟩ [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 2015 ftuniversailles https://doi.org/10.5194/gmd-8-3621-2015 2024-04-04T17:36:58Z International audience We describe the creation of a data set describing changes related to the presence of ice sheets, including ice-sheet extent and height, ice-shelf extent, and the distribution and elevation of ice-free land at the Last Glacial Maximum (LGM), which were used in LGM experiments conducted as part of the fifth phase of the Coupled Modelling Intercomparison Project (CMIP5) and the third phase of the Palaeoclimate Modelling Intercomparison Project (PMIP3). The CMIP5/PMIP3 data sets were created from reconstructions made by three different groups, which were all obtained using a model-inversion approach but differ in the assumptions used in the modelling and in the type of data used as constraints. The ice-sheet extent in the Northern Hemisphere (NH) does not vary substantially between the three individual data sources. The difference in the topography of the NH ice sheets is also moderate, and smaller than the differences between these reconstructions (and the resultant composite reconstruction) and ice-sheet reconstructions used in previous generations of PMIP. Only two of the individual reconstructions provide information for Antarctica. The discrepancy between these two reconstructions is larger than the difference for the NH ice sheets, although still less than the difference between the composite reconstruction and previous PMIP ice-sheet reconstructions. Although largely confined to the ice-covered regions, differences between the climate response to the individual LGM reconstructions extend over the North Atlantic Ocean and Northern Hemisphere continents , partly through atmospheric stationary waves. Differences between the climate response to the CMIP5/PMIP3 composite and any individual ice-sheet reconstruction are smaller than those between the CMIP5/PMIP3 composite and the ice sheet used in the last phase of PMIP (PMIP2). Article in Journal/Newspaper Antarc* Antarctica Ice Sheet Ice Shelf North Atlantic Université de Versailles Saint-Quentin-en-Yvelines: HAL-UVSQ Geoscientific Model Development 8 11 3621 3637