Early detection of anthropogenic climate change signals in the ocean interior

Robust detection of anthropogenic climate change is crucial to: (i) improve our understanding of Earth system responses to external forcing, (ii) reduce uncertainty in future climate projections, and (iii) develop efficient mitigation and adaptation plans. Here, we use Earth system model projections...

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Published in:Scientific Reports
Main Authors: Jerry F. Tjiputra, Jean Negrel, Are Olsen
Format: Article in Journal/Newspaper
Language:unknown
Published: 2023
Subjects:
Online Access:https://zenodo.org/record/7867617
https://doi.org/10.1038/s41598-023-30159-0
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spelling ftzenodo:oai:zenodo.org:7867617 2023-06-11T04:14:30+02:00 Early detection of anthropogenic climate change signals in the ocean interior Jerry F. Tjiputra Jean Negrel Are Olsen 2023-02-21 https://zenodo.org/record/7867617 https://doi.org/10.1038/s41598-023-30159-0 unknown info:eu-repo/grantAgreement/EC/H2020/820989/ info:eu-repo/grantAgreement/EC/H2020/817578/ https://zenodo.org/record/7867617 https://doi.org/10.1038/s41598-023-30159-0 oai:zenodo.org:7867617 info:eu-repo/semantics/openAccess https://creativecommons.org/licenses/by/4.0/legalcode Carbon cycle Climate and Earth system modelling info:eu-repo/semantics/article publication-article 2023 ftzenodo https://doi.org/10.1038/s41598-023-30159-0 2023-05-30T22:57:23Z Robust detection of anthropogenic climate change is crucial to: (i) improve our understanding of Earth system responses to external forcing, (ii) reduce uncertainty in future climate projections, and (iii) develop efficient mitigation and adaptation plans. Here, we use Earth system model projections to establish the detection timescales of anthropogenic signals in the global ocean through analyzing temperature, salinity, oxygen, and pH evolution from surface to 2000 m depths. For most variables, anthropogenic changes emerge earlier in the interior ocean than at the surface, due to the lower background variability at depth. Acidification is detectable earliest, followed by warming and oxygen changes in the subsurface tropical Atlantic. Temperature and salinity changes in the subsurface tropical and subtropical North Atlantic are shown to be early indicators for a slowdown of the Atlantic Meridional Overturning Circulation. Even under mitigated scenarios, inner ocean anthropogenic signals are projected to emerge within the next few decades. This is because they originate from existing surface changes that are now propagating into the interior. In addition to the tropical Atlantic, our study calls for establishment of long-term interior monitoring systems in the Southern Ocean and North Atlantic in order to elucidate how spatially heterogeneous anthropogenic signals propagate into the interior and impact marine ecosystems and biogeochemistry. Article in Journal/Newspaper North Atlantic Southern Ocean Zenodo Southern Ocean Scientific Reports 13 1
institution Open Polar
collection Zenodo
op_collection_id ftzenodo
language unknown
topic Carbon cycle
Climate and Earth system modelling
spellingShingle Carbon cycle
Climate and Earth system modelling
Jerry F. Tjiputra
Jean Negrel
Are Olsen
Early detection of anthropogenic climate change signals in the ocean interior
topic_facet Carbon cycle
Climate and Earth system modelling
description Robust detection of anthropogenic climate change is crucial to: (i) improve our understanding of Earth system responses to external forcing, (ii) reduce uncertainty in future climate projections, and (iii) develop efficient mitigation and adaptation plans. Here, we use Earth system model projections to establish the detection timescales of anthropogenic signals in the global ocean through analyzing temperature, salinity, oxygen, and pH evolution from surface to 2000 m depths. For most variables, anthropogenic changes emerge earlier in the interior ocean than at the surface, due to the lower background variability at depth. Acidification is detectable earliest, followed by warming and oxygen changes in the subsurface tropical Atlantic. Temperature and salinity changes in the subsurface tropical and subtropical North Atlantic are shown to be early indicators for a slowdown of the Atlantic Meridional Overturning Circulation. Even under mitigated scenarios, inner ocean anthropogenic signals are projected to emerge within the next few decades. This is because they originate from existing surface changes that are now propagating into the interior. In addition to the tropical Atlantic, our study calls for establishment of long-term interior monitoring systems in the Southern Ocean and North Atlantic in order to elucidate how spatially heterogeneous anthropogenic signals propagate into the interior and impact marine ecosystems and biogeochemistry.
format Article in Journal/Newspaper
author Jerry F. Tjiputra
Jean Negrel
Are Olsen
author_facet Jerry F. Tjiputra
Jean Negrel
Are Olsen
author_sort Jerry F. Tjiputra
title Early detection of anthropogenic climate change signals in the ocean interior
title_short Early detection of anthropogenic climate change signals in the ocean interior
title_full Early detection of anthropogenic climate change signals in the ocean interior
title_fullStr Early detection of anthropogenic climate change signals in the ocean interior
title_full_unstemmed Early detection of anthropogenic climate change signals in the ocean interior
title_sort early detection of anthropogenic climate change signals in the ocean interior
publishDate 2023
url https://zenodo.org/record/7867617
https://doi.org/10.1038/s41598-023-30159-0
geographic Southern Ocean
geographic_facet Southern Ocean
genre North Atlantic
Southern Ocean
genre_facet North Atlantic
Southern Ocean
op_relation info:eu-repo/grantAgreement/EC/H2020/820989/
info:eu-repo/grantAgreement/EC/H2020/817578/
https://zenodo.org/record/7867617
https://doi.org/10.1038/s41598-023-30159-0
oai:zenodo.org:7867617
op_rights info:eu-repo/semantics/openAccess
https://creativecommons.org/licenses/by/4.0/legalcode
op_doi https://doi.org/10.1038/s41598-023-30159-0
container_title Scientific Reports
container_volume 13
container_issue 1
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