Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S

The Southern Ocean between 30°S and 55°S is a major sink of excess heat and anthropogenic carbon, but model projections of these sinks remain highly uncertain. Reducing such uncertainties is required to effectively guide the development of climate mitigation policies for meeting the ambitious climat...

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Published in:Nature Communications
Main Authors: Bourgeois, Timothée, Goris, Nadine, Schwinger, Jörg, Tjiputra, Jerry F.
Format: Article in Journal/Newspaper
Language:unknown
Published: Zenodo 2022
Subjects:
Online Access:https://doi.org/10.1038/s41467-022-27979-5
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spelling ftzenodo:oai:zenodo.org:5863088 2024-09-15T18:37:02+00:00 Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S Bourgeois, Timothée Goris, Nadine Schwinger, Jörg Tjiputra, Jerry F. 2022-01-17 https://doi.org/10.1038/s41467-022-27979-5 unknown Zenodo https://zenodo.org/communities/eu https://doi.org/10.1038/s41467-022-27979-5 oai:zenodo.org:5863088 info:eu-repo/semantics/openAccess Creative Commons Attribution 4.0 International https://creativecommons.org/licenses/by/4.0/legalcode info:eu-repo/semantics/article 2022 ftzenodo https://doi.org/10.1038/s41467-022-27979-5 2024-07-26T20:15:31Z The Southern Ocean between 30°S and 55°S is a major sink of excess heat and anthropogenic carbon, but model projections of these sinks remain highly uncertain. Reducing such uncertainties is required to effectively guide the development of climate mitigation policies for meeting the ambitious climate targets of the Paris Agreement. Here, we show that the large spread in the projections of future excess heat uptake efficiency and cumulative anthropogenic carbon uptake in this region are strongly linked to the models’ contemporary stratification. This relationship is robust across two generations of Earth system models and is used to reduce the uncertainty of future estimates of the cumulative anthropogenic carbon uptake by up to 53% and the excess heat uptake efficiency by 28%. Our results highlight that, for this region, an improved representation of stratification in Earth system models is key to constrain future carbon budgets and climate change projections. Article in Journal/Newspaper Southern Ocean Zenodo Nature Communications 13 1
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
description The Southern Ocean between 30°S and 55°S is a major sink of excess heat and anthropogenic carbon, but model projections of these sinks remain highly uncertain. Reducing such uncertainties is required to effectively guide the development of climate mitigation policies for meeting the ambitious climate targets of the Paris Agreement. Here, we show that the large spread in the projections of future excess heat uptake efficiency and cumulative anthropogenic carbon uptake in this region are strongly linked to the models’ contemporary stratification. This relationship is robust across two generations of Earth system models and is used to reduce the uncertainty of future estimates of the cumulative anthropogenic carbon uptake by up to 53% and the excess heat uptake efficiency by 28%. Our results highlight that, for this region, an improved representation of stratification in Earth system models is key to constrain future carbon budgets and climate change projections.
format Article in Journal/Newspaper
author Bourgeois, Timothée
Goris, Nadine
Schwinger, Jörg
Tjiputra, Jerry F.
spellingShingle Bourgeois, Timothée
Goris, Nadine
Schwinger, Jörg
Tjiputra, Jerry F.
Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
author_facet Bourgeois, Timothée
Goris, Nadine
Schwinger, Jörg
Tjiputra, Jerry F.
author_sort Bourgeois, Timothée
title Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
title_short Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
title_full Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
title_fullStr Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
title_full_unstemmed Stratification constrains future heat and carbon uptake in the Southern Ocean between 30°S and 55°S
title_sort stratification constrains future heat and carbon uptake in the southern ocean between 30°s and 55°s
publisher Zenodo
publishDate 2022
url https://doi.org/10.1038/s41467-022-27979-5
genre Southern Ocean
genre_facet Southern Ocean
op_relation https://zenodo.org/communities/eu
https://doi.org/10.1038/s41467-022-27979-5
oai:zenodo.org:5863088
op_rights info:eu-repo/semantics/openAccess
Creative Commons Attribution 4.0 International
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1038/s41467-022-27979-5
container_title Nature Communications
container_volume 13
container_issue 1
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