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: Tjiputra, Jerry, Negrel, Jean, Olsen, Are
Format: Article in Journal/Newspaper
Language:English
Published: Nature 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3064429
https://doi.org/10.1038/s41598-023-30159-0
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spelling ftunivbergen:oai:bora.uib.no:11250/3064429 2023-06-11T04:14:30+02:00 Early detection of anthropogenic climate change signals in the ocean interior Tjiputra, Jerry Negrel, Jean Olsen, Are 2023 application/pdf https://hdl.handle.net/11250/3064429 https://doi.org/10.1038/s41598-023-30159-0 eng eng Nature Norges forskningsråd: 275268 Norges forskningsråd: 318477 Norges forskningsråd: 295046 EC/H2020/820989 EC/H2020/817578 urn:issn:2045-2322 https://hdl.handle.net/11250/3064429 https://doi.org/10.1038/s41598-023-30159-0 cristin:2129790 Scientific Reports. 2023, 13, 3006. Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Copyright 2023 The Author(s) 3006 Scientific Reports 13 Journal article Peer reviewed 2023 ftunivbergen https://doi.org/10.1038/s41598-023-30159-0 2023-04-26T23:06:27Z 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. publishedVersion Article in Journal/Newspaper North Atlantic Southern Ocean University of Bergen: Bergen Open Research Archive (BORA-UiB) Southern Ocean Scientific Reports 13 1
institution Open Polar
collection University of Bergen: Bergen Open Research Archive (BORA-UiB)
op_collection_id ftunivbergen
language English
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. publishedVersion
format Article in Journal/Newspaper
author Tjiputra, Jerry
Negrel, Jean
Olsen, Are
spellingShingle Tjiputra, Jerry
Negrel, Jean
Olsen, Are
Early detection of anthropogenic climate change signals in the ocean interior
author_facet Tjiputra, Jerry
Negrel, Jean
Olsen, Are
author_sort Tjiputra, Jerry
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
publisher Nature
publishDate 2023
url https://hdl.handle.net/11250/3064429
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_source 3006
Scientific Reports
13
op_relation Norges forskningsråd: 275268
Norges forskningsråd: 318477
Norges forskningsråd: 295046
EC/H2020/820989
EC/H2020/817578
urn:issn:2045-2322
https://hdl.handle.net/11250/3064429
https://doi.org/10.1038/s41598-023-30159-0
cristin:2129790
Scientific Reports. 2023, 13, 3006.
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
Copyright 2023 The Author(s)
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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