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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Bibliographic Details
Published in:Communications Earth & Environment
Main Authors: Messias, Marie-José, Mercier, Herlé
Other Authors: 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
Language:English
Published: HAL CCSD 2022
Subjects:
[SDU]Sciences of the Universe [physics]
[SDU.STU]Sciences of the Universe [physics]/Earth Sciences
Labrador Sea
Nordic Seas
North Atlantic
Online Access:https://insu.hal.science/insu-03683290
https://insu.hal.science/insu-03683290/document
https://insu.hal.science/insu-03683290/file/s43247-022-00443-4.pdf
https://doi.org/10.1038/s43247-022-00443-4
Description
Summary: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.

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