A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum

Paleoclimate proxy records from the North Atlantic region reveal substantially greater multicentennial temperature variability during the Last Glacial Maximum (LGM) compared to the current interglacial. As there was no obvious change in external forcing, causes for the increased variability remain u...

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Published in:Science Advances
Main Authors: Prange, Matthias, Jonkers, Lukas, Merkel, Ute, Schulz, Michael, Bakker, Pepijn
Format: Article in Journal/Newspaper
Language:English
Published: AAAS (American Association for the Advancement of Science) 2023
Subjects:
Online Access:https://oceanrep.geomar.de/id/eprint/59765/
https://oceanrep.geomar.de/id/eprint/59765/1/Prange.pdf
https://doi.org/10.1126/sciadv.adh1106
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spelling ftoceanrep:oai:oceanrep.geomar.de:59765 2024-02-11T10:06:06+01:00 A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum Prange, Matthias Jonkers, Lukas Merkel, Ute Schulz, Michael Bakker, Pepijn 2023-11-03 text https://oceanrep.geomar.de/id/eprint/59765/ https://oceanrep.geomar.de/id/eprint/59765/1/Prange.pdf https://doi.org/10.1126/sciadv.adh1106 en eng AAAS (American Association for the Advancement of Science) https://oceanrep.geomar.de/id/eprint/59765/1/Prange.pdf Prange, M., Jonkers, L., Merkel, U., Schulz, M. and Bakker, P. (2023) A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum. Science Advances, 9 . Art.Nr. 44. DOI 10.1126/sciadv.adh1106 <https://doi.org/10.1126/sciadv.adh1106>. doi:10.1126/sciadv.adh1106 info:eu-repo/semantics/restrictedAccess Article PeerReviewed 2023 ftoceanrep https://doi.org/10.1126/sciadv.adh1106 2024-01-15T00:28:08Z Paleoclimate proxy records from the North Atlantic region reveal substantially greater multicentennial temperature variability during the Last Glacial Maximum (LGM) compared to the current interglacial. As there was no obvious change in external forcing, causes for the increased variability remain unknown. Exploiting LGM simulations with a comprehensive coupled climate model along with high-resolution proxy records, we introduce an oscillatory mode of multicentennial variability, which is associated with moderate variations in the Atlantic meridional overturning circulation and depends on the large-scale salinity distribution. This self-sustained mode is amplified by sea-ice feedbacks and induces maximum surface temperature variability in the subpolar North Atlantic region. Characterized by a distinct climatic imprint and different dynamics, the multicentennial oscillation has to be distinguished from Dansgaard-Oeschger variability and emerges only under full LGM climate forcing. The potential of multicentennial modes of variability to emerge or disappear in response to changing climate forcing may have implications for future climate change. Article in Journal/Newspaper North Atlantic Sea ice OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel) Science Advances 9 44
institution Open Polar
collection OceanRep (GEOMAR Helmholtz Centre für Ocean Research Kiel)
op_collection_id ftoceanrep
language English
description Paleoclimate proxy records from the North Atlantic region reveal substantially greater multicentennial temperature variability during the Last Glacial Maximum (LGM) compared to the current interglacial. As there was no obvious change in external forcing, causes for the increased variability remain unknown. Exploiting LGM simulations with a comprehensive coupled climate model along with high-resolution proxy records, we introduce an oscillatory mode of multicentennial variability, which is associated with moderate variations in the Atlantic meridional overturning circulation and depends on the large-scale salinity distribution. This self-sustained mode is amplified by sea-ice feedbacks and induces maximum surface temperature variability in the subpolar North Atlantic region. Characterized by a distinct climatic imprint and different dynamics, the multicentennial oscillation has to be distinguished from Dansgaard-Oeschger variability and emerges only under full LGM climate forcing. The potential of multicentennial modes of variability to emerge or disappear in response to changing climate forcing may have implications for future climate change.
format Article in Journal/Newspaper
author Prange, Matthias
Jonkers, Lukas
Merkel, Ute
Schulz, Michael
Bakker, Pepijn
spellingShingle Prange, Matthias
Jonkers, Lukas
Merkel, Ute
Schulz, Michael
Bakker, Pepijn
A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
author_facet Prange, Matthias
Jonkers, Lukas
Merkel, Ute
Schulz, Michael
Bakker, Pepijn
author_sort Prange, Matthias
title A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
title_short A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
title_full A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
title_fullStr A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
title_full_unstemmed A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum
title_sort multicentennial mode of north atlantic climate variability throughout the last glacial maximum
publisher AAAS (American Association for the Advancement of Science)
publishDate 2023
url https://oceanrep.geomar.de/id/eprint/59765/
https://oceanrep.geomar.de/id/eprint/59765/1/Prange.pdf
https://doi.org/10.1126/sciadv.adh1106
genre North Atlantic
Sea ice
genre_facet North Atlantic
Sea ice
op_relation https://oceanrep.geomar.de/id/eprint/59765/1/Prange.pdf
Prange, M., Jonkers, L., Merkel, U., Schulz, M. and Bakker, P. (2023) A multicentennial mode of North Atlantic climate variability throughout the Last Glacial Maximum. Science Advances, 9 . Art.Nr. 44. DOI 10.1126/sciadv.adh1106 <https://doi.org/10.1126/sciadv.adh1106>.
doi:10.1126/sciadv.adh1106
op_rights info:eu-repo/semantics/restrictedAccess
op_doi https://doi.org/10.1126/sciadv.adh1106
container_title Science Advances
container_volume 9
container_issue 44
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