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20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance

The historical evolution of Earth’s energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provid...

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Detalles Bibliográficos
Autores principales: Bagnell, A., DeVries, T.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2021
Materias:
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8322321/
https://www.ncbi.nlm.nih.gov/pubmed/34326319
http://dx.doi.org/10.1038/s41467-021-24472-3
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author Bagnell, A.
DeVries, T.
author_facet Bagnell, A.
DeVries, T.
author_sort Bagnell, A.
collection PubMed
description The historical evolution of Earth’s energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provide a global reconstruction of historical changes in full-depth ocean heat content based on interpolated subsurface temperature data using an autoregressive artificial neural network, providing estimates of total ocean warming for the period 1946-2019. We find that cooling of the deep ocean and a small heat gain in the upper ocean led to no robust trend in global ocean heat content from 1960-1990, implying a roughly balanced Earth energy budget within −0.16 to 0.06 W m(−2) over most of the latter half of the 20th century. However, the past three decades have seen a rapid acceleration in ocean warming, with the entire ocean warming from top to bottom at a rate of 0.63 ± 0.13 W m(−2). These results suggest a delayed onset of a positive Earth energy imbalance relative to previous estimates, although large uncertainties remain.
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spelling pubmed-83223212021-08-03 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance Bagnell, A. DeVries, T. Nat Commun Article The historical evolution of Earth’s energy imbalance can be quantified by changes in the global ocean heat content. However, historical reconstructions of ocean heat content often neglect a large volume of the deep ocean, due to sparse observations of ocean temperatures below 2000 m. Here, we provide a global reconstruction of historical changes in full-depth ocean heat content based on interpolated subsurface temperature data using an autoregressive artificial neural network, providing estimates of total ocean warming for the period 1946-2019. We find that cooling of the deep ocean and a small heat gain in the upper ocean led to no robust trend in global ocean heat content from 1960-1990, implying a roughly balanced Earth energy budget within −0.16 to 0.06 W m(−2) over most of the latter half of the 20th century. However, the past three decades have seen a rapid acceleration in ocean warming, with the entire ocean warming from top to bottom at a rate of 0.63 ± 0.13 W m(−2). These results suggest a delayed onset of a positive Earth energy imbalance relative to previous estimates, although large uncertainties remain. Nature Publishing Group UK 2021-07-29 /pmc/articles/PMC8322321/ /pubmed/34326319 http://dx.doi.org/10.1038/s41467-021-24472-3 Text en © The Author(s) 2021 https://creativecommons.org/licenses/by/4.0/Open Access This article is licensed under a Creative Commons Attribution 4.0 International License, which permits use, sharing, adaptation, distribution and reproduction in any medium or format, as long as you give appropriate credit to the original author(s) and the source, provide a link to the Creative Commons license, and indicate if changes were made. The images or other third party material in this article are included in the article’s Creative Commons license, unless indicated otherwise in a credit line to the material. If material is not included in the article’s Creative Commons license and your intended use is not permitted by statutory regulation or exceeds the permitted use, you will need to obtain permission directly from the copyright holder. To view a copy of this license, visit http://creativecommons.org/licenses/by/4.0/ (https://creativecommons.org/licenses/by/4.0/) .
spellingShingle Article
Bagnell, A.
DeVries, T.
20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title_full 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title_fullStr 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title_full_unstemmed 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title_short 20(th) century cooling of the deep ocean contributed to delayed acceleration of Earth’s energy imbalance
title_sort 20(th) century cooling of the deep ocean contributed to delayed acceleration of earth’s energy imbalance
topic Article
url https://www.ncbi.nlm.nih.gov/pmc/articles/PMC8322321/
https://www.ncbi.nlm.nih.gov/pubmed/34326319
http://dx.doi.org/10.1038/s41467-021-24472-3
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