The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic
International audience Understanding ocean excess heat uptake is crucial for assessing climate warming, yet uncertainties remain about its history and redistribution. Here, we reconstruct ocean heat content change along the 25°N Atlantic hydrographic section and assess its spatiotemporal origin and...
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ftinsu:oai:HAL:hal-03814734v1 2024-04-14T08:14:31+00:00 The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic Messias, Marie-José Mercier, Herlé University of Exeter Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) 2022 https://hal.science/hal-03814734 https://hal.science/hal-03814734/document https://hal.science/hal-03814734/file/messias_mercier_2022_cee.pdf https://doi.org/10.1038/s43247-022-00443-4 en eng HAL CCSD Springer Nature info:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-022-00443-4 hal-03814734 https://hal.science/hal-03814734 https://hal.science/hal-03814734/document https://hal.science/hal-03814734/file/messias_mercier_2022_cee.pdf doi:10.1038/s43247-022-00443-4 info:eu-repo/semantics/OpenAccess ISSN: 2662-4435 Communications Earth & Environment https://hal.science/hal-03814734 Communications Earth & Environment, 2022, 3 (1), pp.118. ⟨10.1038/s43247-022-00443-4⟩ [SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography info:eu-repo/semantics/article Journal articles 2022 ftinsu https://doi.org/10.1038/s43247-022-00443-4 2024-03-21T17:10:21Z International audience Understanding ocean excess heat uptake is crucial for assessing climate warming, yet uncertainties remain about its history and redistribution. Here, we reconstruct ocean heat content change along the 25°N Atlantic hydrographic section and assess its spatiotemporal origin and fate. We show that the delayed response of the ocean below 700 m to sea surface temperature change contribute to 62% of full depth warming at this latitude for 1850–2018, falling to 35% for 1975–2018 when anthropogenic warming in the upper ocean accelerated. The regional climate fluctuations shape ocean heat content variability at 25°N with contributions from the Labrador Sea producing most of the decadal variability and the Nordic Seas bound to become the main contributor to deep ocean warming in the coming decades. Chiefly, the net excess heat transport across 25°N has increased recently, warming the domain north of 25°N at a rate of 0.89 ± 0.19 W m −2 during 2012–2018, revealing that excess heat redistribution is a key driver of North Atlantic heat gain. Article in Journal/Newspaper Labrador Sea Nordic Seas North Atlantic Institut national des sciences de l'Univers: HAL-INSU Communications Earth & Environment 3 1 |
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Open Polar |
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Institut national des sciences de l'Univers: HAL-INSU |
op_collection_id |
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language |
English |
topic |
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
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[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography Messias, Marie-José Mercier, Herlé The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
topic_facet |
[SDU.STU.CL]Sciences of the Universe [physics]/Earth Sciences/Climatology [SDU.STU.OC]Sciences of the Universe [physics]/Earth Sciences/Oceanography |
description |
International audience Understanding ocean excess heat uptake is crucial for assessing climate warming, yet uncertainties remain about its history and redistribution. Here, we reconstruct ocean heat content change along the 25°N Atlantic hydrographic section and assess its spatiotemporal origin and fate. We show that the delayed response of the ocean below 700 m to sea surface temperature change contribute to 62% of full depth warming at this latitude for 1850–2018, falling to 35% for 1975–2018 when anthropogenic warming in the upper ocean accelerated. The regional climate fluctuations shape ocean heat content variability at 25°N with contributions from the Labrador Sea producing most of the decadal variability and the Nordic Seas bound to become the main contributor to deep ocean warming in the coming decades. Chiefly, the net excess heat transport across 25°N has increased recently, warming the domain north of 25°N at a rate of 0.89 ± 0.19 W m −2 during 2012–2018, revealing that excess heat redistribution is a key driver of North Atlantic heat gain. |
author2 |
University of Exeter Laboratoire d'Océanographie Physique et Spatiale (LOPS) Institut de Recherche pour le Développement (IRD)-Institut Français de Recherche pour l'Exploitation de la Mer (IFREMER)-Institut national des sciences de l'Univers (INSU - CNRS)-Université de Brest (UBO)-Centre National de la Recherche Scientifique (CNRS) |
format |
Article in Journal/Newspaper |
author |
Messias, Marie-José Mercier, Herlé |
author_facet |
Messias, Marie-José Mercier, Herlé |
author_sort |
Messias, Marie-José |
title |
The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
title_short |
The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
title_full |
The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
title_fullStr |
The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
title_full_unstemmed |
The redistribution of anthropogenic excess heat is a key driver of warming in the North Atlantic |
title_sort |
redistribution of anthropogenic excess heat is a key driver of warming in the north atlantic |
publisher |
HAL CCSD |
publishDate |
2022 |
url |
https://hal.science/hal-03814734 https://hal.science/hal-03814734/document https://hal.science/hal-03814734/file/messias_mercier_2022_cee.pdf https://doi.org/10.1038/s43247-022-00443-4 |
genre |
Labrador Sea Nordic Seas North Atlantic |
genre_facet |
Labrador Sea Nordic Seas North Atlantic |
op_source |
ISSN: 2662-4435 Communications Earth & Environment https://hal.science/hal-03814734 Communications Earth & Environment, 2022, 3 (1), pp.118. ⟨10.1038/s43247-022-00443-4⟩ |
op_relation |
info:eu-repo/semantics/altIdentifier/doi/10.1038/s43247-022-00443-4 hal-03814734 https://hal.science/hal-03814734 https://hal.science/hal-03814734/document https://hal.science/hal-03814734/file/messias_mercier_2022_cee.pdf doi:10.1038/s43247-022-00443-4 |
op_rights |
info:eu-repo/semantics/OpenAccess |
op_doi |
https://doi.org/10.1038/s43247-022-00443-4 |
container_title |
Communications Earth & Environment |
container_volume |
3 |
container_issue |
1 |
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1796312703311020032 |