Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium

International audience Estimated external radiative forcings, model results, and proxy-based climate reconstructions have been used over the past several decades to improve our understanding of the mechanisms underlying observed climate variability and change over the past millennium. Here, the rece...

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Published in:Climate of the Past
Main Authors: 2k-PMIP3, PAGES, Bothe, O., Evans, M., Donado, L. Fernández, Bustamante, E. Garcia, Gergis, J., Gonzalez-Rouco, J. F., Hegerl, G., Hind, A., Jungclaus, J., Kaufman, D., Lehner, F., McKay, N., Moberg, A., Raible, C. C., Schurer, A., Shi, F., Smerdon, J. E., Gunten, L. von, Wagner, S., Warren, E., Widmann, M., Yiou, P., Zorita, E., Goosse, H.
Other Authors: Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ), Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR), Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2015
Subjects:
Online Access:https://hal.archives-ouvertes.fr/hal-03263553
https://hal.archives-ouvertes.fr/hal-03263553/document
https://hal.archives-ouvertes.fr/hal-03263553/file/cp-11-1673-2015.pdf
https://doi.org/10.5194/cp-11-1673-2015
id ftccsdartic:oai:HAL:hal-03263553v1
record_format openpolar
institution Open Polar
collection Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe)
op_collection_id ftccsdartic
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
2k-PMIP3, PAGES
Bothe, O.
Evans, M.
Donado, L. Fernández
Bustamante, E. Garcia
Gergis, J.
Gonzalez-Rouco, J. F.
Hegerl, G.
Hind, A.
Jungclaus, J.
Kaufman, D.
Lehner, F.
McKay, N.
Moberg, A.
Raible, C. C.
Schurer, A.
Shi, F.
Smerdon, J. E.
Gunten, L. von
Wagner, S.
Warren, E.
Widmann, M.
Yiou, P.
Zorita, E.
Goosse, H.
Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.ENVI]Sciences of the Universe [physics]/Continental interfaces
environment
description International audience Estimated external radiative forcings, model results, and proxy-based climate reconstructions have been used over the past several decades to improve our understanding of the mechanisms underlying observed climate variability and change over the past millennium. Here, the recent set of temperature reconstructions at the continentalscale generated by the PAGES 2k project and a collection of state-of-the-art model simulations driven by realistic external forcings are jointly analysed. The first aim is to estimate the consistency between model results and reconstructions for each continental-scale region over the time and frequency domains. Secondly, the links between regions are investigated to determine whether reconstructed global-scale covariability patterns are similar to those identified in model simulations. The third aim is to assess the role of external forcings in the observed temperature variations. From a large set of analyses, we conclude that models are in relatively good agreement with temperature reconstructions for Northern Hemisphere regions, particularly in the Arctic. This is likely due to the relatively large amplitude of the externally forced response across northern and high-latitude regions, which results in a clearly detectable signature in both reconstructions and simulations. Conversely, models disagree strongly with the reconstructions in the Southern Hemisphere. Furthermore, the simulations are more regionally coherent than the reconstructions, perhaps due to an underestimation of the magnitude of internal variability in models or to an overestimation of the response to the external forcing in the Southern Hemisphere. Part of the disagreement might also reflect large uncertainties in the reconstructions, specifically in some Southern Hemisphere regions, which are based on fewer palaeoclimate records than in the Northern Hemisphere.
author2 Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR)
Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ)
format Article in Journal/Newspaper
author 2k-PMIP3, PAGES
Bothe, O.
Evans, M.
Donado, L. Fernández
Bustamante, E. Garcia
Gergis, J.
Gonzalez-Rouco, J. F.
Hegerl, G.
Hind, A.
Jungclaus, J.
Kaufman, D.
Lehner, F.
McKay, N.
Moberg, A.
Raible, C. C.
Schurer, A.
Shi, F.
Smerdon, J. E.
Gunten, L. von
Wagner, S.
Warren, E.
Widmann, M.
Yiou, P.
Zorita, E.
Goosse, H.
author_facet 2k-PMIP3, PAGES
Bothe, O.
Evans, M.
Donado, L. Fernández
Bustamante, E. Garcia
Gergis, J.
Gonzalez-Rouco, J. F.
Hegerl, G.
Hind, A.
Jungclaus, J.
Kaufman, D.
Lehner, F.
McKay, N.
Moberg, A.
Raible, C. C.
Schurer, A.
Shi, F.
Smerdon, J. E.
Gunten, L. von
Wagner, S.
Warren, E.
Widmann, M.
Yiou, P.
Zorita, E.
Goosse, H.
author_sort 2k-PMIP3, PAGES
title Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
title_short Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
title_full Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
title_fullStr Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
title_full_unstemmed Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium
title_sort continental-scale temperature variability in pmip3 simulations and pages 2k regional temperature reconstructions over the past millennium
publisher HAL CCSD
publishDate 2015
url https://hal.archives-ouvertes.fr/hal-03263553
https://hal.archives-ouvertes.fr/hal-03263553/document
https://hal.archives-ouvertes.fr/hal-03263553/file/cp-11-1673-2015.pdf
https://doi.org/10.5194/cp-11-1673-2015
geographic Arctic
geographic_facet Arctic
genre Arctic
genre_facet Arctic
op_source ISSN: 1814-9324
EISSN: 1814-9332
Climate of the Past
https://hal.archives-ouvertes.fr/hal-03263553
Climate of the Past, European Geosciences Union (EGU), 2015, 11 (12), pp.1673 - 1699. ⟨10.5194/cp-11-1673-2015⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-11-1673-2015
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https://hal.archives-ouvertes.fr/hal-03263553
https://hal.archives-ouvertes.fr/hal-03263553/document
https://hal.archives-ouvertes.fr/hal-03263553/file/cp-11-1673-2015.pdf
doi:10.5194/cp-11-1673-2015
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/cp-11-1673-2015
container_title Climate of the Past
container_volume 11
container_issue 12
container_start_page 1673
op_container_end_page 1699
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spelling ftccsdartic:oai:HAL:hal-03263553v1 2023-05-15T15:13:09+02:00 Continental-scale temperature variability in PMIP3 simulations and PAGES 2k regional temperature reconstructions over the past millennium 2k-PMIP3, PAGES Bothe, O. Evans, M. Donado, L. Fernández Bustamante, E. Garcia Gergis, J. Gonzalez-Rouco, J. F. Hegerl, G. Hind, A. Jungclaus, J. Kaufman, D. Lehner, F. McKay, N. Moberg, A. Raible, C. C. Schurer, A. Shi, F. Smerdon, J. E. Gunten, L. von Wagner, S. Warren, E. Widmann, M. Yiou, P. Zorita, E. Goosse, H. Laboratoire des Sciences du Climat et de l'Environnement Gif-sur-Yvette (LSCE) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) Extrèmes : Statistiques, Impacts et Régionalisation (ESTIMR) Institut national des sciences de l'Univers (INSU - CNRS)-Université Paris-Saclay-Centre National de la Recherche Scientifique (CNRS)-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)-Commissariat à l'énergie atomique et aux énergies alternatives (CEA)-Université de Versailles Saint-Quentin-en-Yvelines (UVSQ) 2015-12-16 https://hal.archives-ouvertes.fr/hal-03263553 https://hal.archives-ouvertes.fr/hal-03263553/document https://hal.archives-ouvertes.fr/hal-03263553/file/cp-11-1673-2015.pdf https://doi.org/10.5194/cp-11-1673-2015 en eng HAL CCSD European Geosciences Union (EGU) info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-11-1673-2015 hal-03263553 https://hal.archives-ouvertes.fr/hal-03263553 https://hal.archives-ouvertes.fr/hal-03263553/document https://hal.archives-ouvertes.fr/hal-03263553/file/cp-11-1673-2015.pdf doi:10.5194/cp-11-1673-2015 info:eu-repo/semantics/OpenAccess ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.archives-ouvertes.fr/hal-03263553 Climate of the Past, European Geosciences Union (EGU), 2015, 11 (12), pp.1673 - 1699. ⟨10.5194/cp-11-1673-2015⟩ [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 ftccsdartic https://doi.org/10.5194/cp-11-1673-2015 2021-12-19T00:03:29Z International audience Estimated external radiative forcings, model results, and proxy-based climate reconstructions have been used over the past several decades to improve our understanding of the mechanisms underlying observed climate variability and change over the past millennium. Here, the recent set of temperature reconstructions at the continentalscale generated by the PAGES 2k project and a collection of state-of-the-art model simulations driven by realistic external forcings are jointly analysed. The first aim is to estimate the consistency between model results and reconstructions for each continental-scale region over the time and frequency domains. Secondly, the links between regions are investigated to determine whether reconstructed global-scale covariability patterns are similar to those identified in model simulations. The third aim is to assess the role of external forcings in the observed temperature variations. From a large set of analyses, we conclude that models are in relatively good agreement with temperature reconstructions for Northern Hemisphere regions, particularly in the Arctic. This is likely due to the relatively large amplitude of the externally forced response across northern and high-latitude regions, which results in a clearly detectable signature in both reconstructions and simulations. Conversely, models disagree strongly with the reconstructions in the Southern Hemisphere. Furthermore, the simulations are more regionally coherent than the reconstructions, perhaps due to an underestimation of the magnitude of internal variability in models or to an overestimation of the response to the external forcing in the Southern Hemisphere. Part of the disagreement might also reflect large uncertainties in the reconstructions, specifically in some Southern Hemisphere regions, which are based on fewer palaeoclimate records than in the Northern Hemisphere. Article in Journal/Newspaper Arctic Archive ouverte HAL (Hyper Article en Ligne, CCSD - Centre pour la Communication Scientifique Directe) Arctic Climate of the Past 11 12 1673 1699