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...

Full description

Bibliographic Details
Published in:Scientific Reports
Main Authors: Tjiputra, Jerry, Negrel, Jean, Olsen, Are
Format: Article in Journal/Newspaper
Language:English
Published: 2023
Subjects:
Online Access:https://hdl.handle.net/11250/3061656
https://doi.org/10.1038/s41598-023-30159-0
id ftnorce:oai:norceresearch.brage.unit.no:11250/3061656
record_format openpolar
spelling ftnorce:oai:norceresearch.brage.unit.no:11250/3061656 2023-05-15T17:30:37+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/11250/3061656 https://doi.org/10.1038/s41598-023-30159-0 eng eng Norges forskningsråd: 275268 Norges forskningsråd: 318477 Norges forskningsråd: 295046 EC/H2020/820989 EC/H2020/817578 Scientific Reports. 2023, 13:3006 1-14. urn:issn:2045-2322 https://hdl.handle.net/11250/3061656 https://doi.org/10.1038/s41598-023-30159-0 cristin:2129790 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no Scientific Reports 13:3006 1-14 Journal article Peer reviewed 2023 ftnorce https://doi.org/10.1038/s41598-023-30159-0 2023-04-05T22:47:56Z 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 NORCE vitenarkiv (Norwegian Research Centre) Southern Ocean Scientific Reports 13 1
institution Open Polar
collection NORCE vitenarkiv (Norwegian Research Centre)
op_collection_id ftnorce
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
publishDate 2023
url https://hdl.handle.net/11250/3061656
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 Scientific Reports
13:3006
1-14
op_relation Norges forskningsråd: 275268
Norges forskningsråd: 318477
Norges forskningsråd: 295046
EC/H2020/820989
EC/H2020/817578
Scientific Reports. 2023, 13:3006 1-14.
urn:issn:2045-2322
https://hdl.handle.net/11250/3061656
https://doi.org/10.1038/s41598-023-30159-0
cristin:2129790
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
op_doi https://doi.org/10.1038/s41598-023-30159-0
container_title Scientific Reports
container_volume 13
container_issue 1
_version_ 1766127477033271296