Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events

International audience Dansgaard–Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based...

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Published in:Climate of the Past
Main Authors: Wary, Mélanie, Eynaud, Frédérique, Swingedouw, Didier, Masson-Delmotte, Valérie, Matthiessen, Jens, Kissel, Catherine, Zumaque, Jena, Rossignol, Linda, Jouzel, Jean
Other Authors: Environnements et Paléoenvironnements OCéaniques (EPOC), Observatoire aquitain des sciences de l'univers (OASU), Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE), Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-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)-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), Glaces et Continents, Climats et Isotopes Stables (GLACCIOS), 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)), Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI), Helmholtz-Gemeinschaft = Helmholtz Association, Climat et Magnétisme (CLIMAG)
Format: Article in Journal/Newspaper
Language:English
Published: HAL CCSD 2017
Subjects:
Online Access:https://hal.science/hal-01584277
https://hal.science/hal-01584277/document
https://hal.science/hal-01584277/file/cp-13-729-2017.pdf
https://doi.org/10.5194/cp-13-729-2017
id ftceafr:oai:HAL:hal-01584277v1
record_format openpolar
institution Open Polar
collection HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives)
op_collection_id ftceafr
language English
topic [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
spellingShingle [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
Wary, Mélanie
Eynaud, Frédérique
Swingedouw, Didier
Masson-Delmotte, Valérie
Matthiessen, Jens
Kissel, Catherine
Zumaque, Jena
Rossignol, Linda
Jouzel, Jean
Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
topic_facet [SDU.OCEAN]Sciences of the Universe [physics]/Ocean
Atmosphere
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology
description International audience Dansgaard–Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based on dinocyst analyses from the 48–30 ka interval of four sediment cores from the northern Northeast Atlantic and southern Norwegian Sea, we provide direct and quantitative evidence of a regional paradoxical seesaw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases. Combined with additional palaeorecords and multi-model hosing simulations , our results suggest that during cold Greenland phases, reduced Atlantic meridional overturning circulation and cold North Atlantic sea-surface conditions were accompanied by the subsurface propagation of warm Atlantic waters that re-emerged in the Nordic Seas and provided moisture towards Greenland summit.
author2 Environnements et Paléoenvironnements OCéaniques (EPOC)
Observatoire aquitain des sciences de l'univers (OASU)
Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE)
Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-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)-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)
Glaces et Continents, Climats et Isotopes Stables (GLACCIOS)
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))
Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI)
Helmholtz-Gemeinschaft = Helmholtz Association
Climat et Magnétisme (CLIMAG)
format Article in Journal/Newspaper
author Wary, Mélanie
Eynaud, Frédérique
Swingedouw, Didier
Masson-Delmotte, Valérie
Matthiessen, Jens
Kissel, Catherine
Zumaque, Jena
Rossignol, Linda
Jouzel, Jean
author_facet Wary, Mélanie
Eynaud, Frédérique
Swingedouw, Didier
Masson-Delmotte, Valérie
Matthiessen, Jens
Kissel, Catherine
Zumaque, Jena
Rossignol, Linda
Jouzel, Jean
author_sort Wary, Mélanie
title Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
title_short Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
title_full Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
title_fullStr Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
title_full_unstemmed Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events
title_sort regional seesaw between the north atlantic and nordic seas during the last glacial abrupt climate events
publisher HAL CCSD
publishDate 2017
url https://hal.science/hal-01584277
https://hal.science/hal-01584277/document
https://hal.science/hal-01584277/file/cp-13-729-2017.pdf
https://doi.org/10.5194/cp-13-729-2017
geographic Greenland
Norwegian Sea
geographic_facet Greenland
Norwegian Sea
genre Greenland
Nordic Seas
North Atlantic
Northeast Atlantic
Norwegian Sea
Sea ice
genre_facet Greenland
Nordic Seas
North Atlantic
Northeast Atlantic
Norwegian Sea
Sea ice
op_source ISSN: 1814-9324
EISSN: 1814-9332
Climate of the Past
https://hal.science/hal-01584277
Climate of the Past, 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩
op_relation info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-13-729-2017
hal-01584277
https://hal.science/hal-01584277
https://hal.science/hal-01584277/document
https://hal.science/hal-01584277/file/cp-13-729-2017.pdf
doi:10.5194/cp-13-729-2017
op_rights info:eu-repo/semantics/OpenAccess
op_doi https://doi.org/10.5194/cp-13-729-2017
container_title Climate of the Past
container_volume 13
container_issue 6
container_start_page 729
op_container_end_page 739
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spelling ftceafr:oai:HAL:hal-01584277v1 2024-06-09T07:46:19+00:00 Regional seesaw between the North Atlantic and Nordic Seas during the last glacial abrupt climate events Wary, Mélanie Eynaud, Frédérique Swingedouw, Didier Masson-Delmotte, Valérie Matthiessen, Jens Kissel, Catherine Zumaque, Jena Rossignol, Linda Jouzel, Jean Environnements et Paléoenvironnements OCéaniques (EPOC) Observatoire aquitain des sciences de l'univers (OASU) Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-Université Sciences et Technologies - Bordeaux 1 (UB)-Institut national des sciences de l'Univers (INSU - CNRS)-Centre National de la Recherche Scientifique (CNRS)-École Pratique des Hautes Études (EPHE) Université Paris Sciences et Lettres (PSL)-Université Paris Sciences et Lettres (PSL)-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)-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) Glaces et Continents, Climats et Isotopes Stables (GLACCIOS) 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)) Alfred-Wegener-Institut, Helmholtz-Zentrum für Polar- und Meeresforschung = Alfred Wegener Institute for Polar and Marine Research = Institut Alfred-Wegener pour la recherche polaire et marine (AWI) Helmholtz-Gemeinschaft = Helmholtz Association Climat et Magnétisme (CLIMAG) 2017 https://hal.science/hal-01584277 https://hal.science/hal-01584277/document https://hal.science/hal-01584277/file/cp-13-729-2017.pdf https://doi.org/10.5194/cp-13-729-2017 en eng HAL CCSD European Geosciences Union (EGU) info:eu-repo/semantics/altIdentifier/doi/10.5194/cp-13-729-2017 hal-01584277 https://hal.science/hal-01584277 https://hal.science/hal-01584277/document https://hal.science/hal-01584277/file/cp-13-729-2017.pdf doi:10.5194/cp-13-729-2017 info:eu-repo/semantics/OpenAccess ISSN: 1814-9324 EISSN: 1814-9332 Climate of the Past https://hal.science/hal-01584277 Climate of the Past, 2017, 13 (6), pp.729-739. ⟨10.5194/cp-13-729-2017⟩ [SDU.OCEAN]Sciences of the Universe [physics]/Ocean Atmosphere [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology info:eu-repo/semantics/article Journal articles 2017 ftceafr https://doi.org/10.5194/cp-13-729-2017 2024-05-16T15:28:21Z International audience Dansgaard–Oeschger oscillations constitute one of the most enigmatic features of the last glacial cycle. Their cold atmospheric phases have been commonly associated with cold sea-surface temperatures and expansion of sea ice in the North Atlantic and adjacent seas. Here, based on dinocyst analyses from the 48–30 ka interval of four sediment cores from the northern Northeast Atlantic and southern Norwegian Sea, we provide direct and quantitative evidence of a regional paradoxical seesaw pattern: cold Greenland and North Atlantic phases coincide with warmer sea-surface conditions and shorter seasonal sea-ice cover durations in the Norwegian Sea as compared to warm phases. Combined with additional palaeorecords and multi-model hosing simulations , our results suggest that during cold Greenland phases, reduced Atlantic meridional overturning circulation and cold North Atlantic sea-surface conditions were accompanied by the subsurface propagation of warm Atlantic waters that re-emerged in the Nordic Seas and provided moisture towards Greenland summit. Article in Journal/Newspaper Greenland Nordic Seas North Atlantic Northeast Atlantic Norwegian Sea Sea ice HAL-CEA (Commissariat à l'énergie atomique et aux énergies alternatives) Greenland Norwegian Sea Climate of the Past 13 6 729 739