The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability
The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical role in ocean circulation and climate change, yet its variability during the last glacial period is poorly documented. Here, we investigate the northward-flowing Glacial Eastern Boundary Current (GEBC) in the...
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ftoskarbordeaux:oai:oskar-bordeaux.fr:20.500.12278/199989 2024-06-23T07:53:46+00:00 The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability TOUCANNE, Samuel SOULET, Guillaume VÁZQUEZ RIVEIROS, Natalia BOSWELL, Steven DENNIELOU, Bernard WAELBROECK, Claire BAYON, Germain MOJTAHID, Meryem BOSQ, Mathieu SABINE, Marjolaine ZARAGOSI, Sebastien BOURILLET, Jean‐françois MERCIER, Herlé 2021-03 https://oskar-bordeaux.fr/handle/20.500.12278/199989 https://hdl.handle.net/20.500.12278/199989 https://doi.org/10.1029/2020PA004068 EN eng 2572-4525 https://oskar-bordeaux.fr/handle/20.500.12278/199989 doi:10.1029/2020PA004068 open http://hal.archives-ouvertes.fr/licences/copyright/ Pas de Licence CC Sciences de l'environnement Planète et Univers [physics] Article de revue 2021 ftoskarbordeaux https://doi.org/20.500.12278/19998910.1029/2020PA004068 2024-05-27T14:03:58Z The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical role in ocean circulation and climate change, yet its variability during the last glacial period is poorly documented. Here, we investigate the northward-flowing Glacial Eastern Boundary Current (GEBC) in the North Atlantic, known today as the European Slope Current, and representing the easternmost portion of the upper branch of the AMOC. Based on flow speed and isotopic records, we show that Dansgaard-Oeschger (D-O) interstadials (stadials) correspond to a faster (weaker) GEBC during the ∼50–15 ka period. This, by analogy to present-day conditions, suggests enhanced (reduced) strength of the subpolar gyre and, by extension, of northern-sourced water production and AMOC during D-O interstadials (stadials). Concomitant fluctuations of both the GEBC and the European Ice Sheet between ∼30 and 17 ka suggest an active role of the upper branch of AMOC in the poleward transport of heat and freshwater to the northern North Atlantic, with direct impacts on deep water formation and AMOC strength. We explore these ice-sheet—AMOC interactions and the associated abrupt climate changes over the last glacial period and the last deglaciation. LabexMER Marine Excellence Research: a changing ocean Tsunamis en Atlantique et MaNche : Définition des Effets par Modélisation Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration Article in Journal/Newspaper Ice Sheet North Atlantic OSKAR Bordeaux (Open Science Knowledge ARchive) Paleoceanography and Paleoclimatology 36 3 |
institution |
Open Polar |
collection |
OSKAR Bordeaux (Open Science Knowledge ARchive) |
op_collection_id |
ftoskarbordeaux |
language |
English |
topic |
Sciences de l'environnement Planète et Univers [physics] |
spellingShingle |
Sciences de l'environnement Planète et Univers [physics] TOUCANNE, Samuel SOULET, Guillaume VÁZQUEZ RIVEIROS, Natalia BOSWELL, Steven DENNIELOU, Bernard WAELBROECK, Claire BAYON, Germain MOJTAHID, Meryem BOSQ, Mathieu SABINE, Marjolaine ZARAGOSI, Sebastien BOURILLET, Jean‐françois MERCIER, Herlé The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
topic_facet |
Sciences de l'environnement Planète et Univers [physics] |
description |
The upper branch of the Atlantic meridional overturning circulation (AMOC) plays a critical role in ocean circulation and climate change, yet its variability during the last glacial period is poorly documented. Here, we investigate the northward-flowing Glacial Eastern Boundary Current (GEBC) in the North Atlantic, known today as the European Slope Current, and representing the easternmost portion of the upper branch of the AMOC. Based on flow speed and isotopic records, we show that Dansgaard-Oeschger (D-O) interstadials (stadials) correspond to a faster (weaker) GEBC during the ∼50–15 ka period. This, by analogy to present-day conditions, suggests enhanced (reduced) strength of the subpolar gyre and, by extension, of northern-sourced water production and AMOC during D-O interstadials (stadials). Concomitant fluctuations of both the GEBC and the European Ice Sheet between ∼30 and 17 ka suggest an active role of the upper branch of AMOC in the poleward transport of heat and freshwater to the northern North Atlantic, with direct impacts on deep water formation and AMOC strength. We explore these ice-sheet—AMOC interactions and the associated abrupt climate changes over the last glacial period and the last deglaciation. LabexMER Marine Excellence Research: a changing ocean Tsunamis en Atlantique et MaNche : Définition des Effets par Modélisation Elucidating the Causes and Effects of Atlantic Circulation Changes through Model-Data Integration |
format |
Article in Journal/Newspaper |
author |
TOUCANNE, Samuel SOULET, Guillaume VÁZQUEZ RIVEIROS, Natalia BOSWELL, Steven DENNIELOU, Bernard WAELBROECK, Claire BAYON, Germain MOJTAHID, Meryem BOSQ, Mathieu SABINE, Marjolaine ZARAGOSI, Sebastien BOURILLET, Jean‐françois MERCIER, Herlé |
author_facet |
TOUCANNE, Samuel SOULET, Guillaume VÁZQUEZ RIVEIROS, Natalia BOSWELL, Steven DENNIELOU, Bernard WAELBROECK, Claire BAYON, Germain MOJTAHID, Meryem BOSQ, Mathieu SABINE, Marjolaine ZARAGOSI, Sebastien BOURILLET, Jean‐françois MERCIER, Herlé |
author_sort |
TOUCANNE, Samuel |
title |
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
title_short |
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
title_full |
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
title_fullStr |
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
title_full_unstemmed |
The North Atlantic Glacial Eastern Boundary Current as a Key Driver for Ice‐Sheet—AMOC Interactions and Climate Instability |
title_sort |
north atlantic glacial eastern boundary current as a key driver for ice‐sheet—amoc interactions and climate instability |
publishDate |
2021 |
url |
https://oskar-bordeaux.fr/handle/20.500.12278/199989 https://hdl.handle.net/20.500.12278/199989 https://doi.org/10.1029/2020PA004068 |
genre |
Ice Sheet North Atlantic |
genre_facet |
Ice Sheet North Atlantic |
op_relation |
2572-4525 https://oskar-bordeaux.fr/handle/20.500.12278/199989 doi:10.1029/2020PA004068 |
op_rights |
open http://hal.archives-ouvertes.fr/licences/copyright/ Pas de Licence CC |
op_doi |
https://doi.org/20.500.12278/19998910.1029/2020PA004068 |
container_title |
Paleoceanography and Paleoclimatology |
container_volume |
36 |
container_issue |
3 |
_version_ |
1802645587761299456 |