Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing

Anthropogenic climate change footprints in the ocean go beyond the mixed layer depth, with considerable impacts throughout mesopelagic and deep-ocean ecosystems. Yet, little is known about the timing of these environmental changes, their spatial extent, and the associated timescales of recovery in t...

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Published in:Journal of Geophysical Research: Oceans
Main Authors: Bertini, Leonardo, Tjiputra, Jerry
Format: Article in Journal/Newspaper
Language:English
Published: 2022
Subjects:
Online Access:https://hdl.handle.net/11250/2996935
https://doi.org/10.1029/2021JC017929
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spelling ftnorce:oai:norceresearch.brage.unit.no:11250/2996935 2023-05-15T17:29:19+02:00 Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing Bertini, Leonardo Tjiputra, Jerry 2022 application/pdf https://hdl.handle.net/11250/2996935 https://doi.org/10.1029/2021JC017929 eng eng Norges forskningsråd: 275268 Norges forskningsråd: 318477 EC/H2020/869357 Journal of Geophysical Research (JGR): Oceans. 2022, 127 (4), 1-22. urn:issn:2169-9275 https://hdl.handle.net/11250/2996935 https://doi.org/10.1029/2021JC017929 cristin:2021572 Navngivelse 4.0 Internasjonal http://creativecommons.org/licenses/by/4.0/deed.no © 2022, The Authors CC-BY Journal of Geophysical Research (JGR): Oceans 127 4 1-22 Peer reviewed Journal article 2022 ftnorce https://doi.org/10.1029/2021JC017929 2022-10-13T05:50:16Z Anthropogenic climate change footprints in the ocean go beyond the mixed layer depth, with considerable impacts throughout mesopelagic and deep-ocean ecosystems. Yet, little is known about the timing of these environmental changes, their spatial extent, and the associated timescales of recovery in the ocean interior when strong mitigation strategies are involved. Here, we simulate idealized rapid climate change and mitigation scenarios using the Norwegian Earth System Model to investigate timescales of climate change onset and recovery and the extent of change in the North Atlantic (NAtl) interior relative to Pre-industrial (PI) variability across a suite of environmental drivers (Temperature—Temp; pH; Dissolved Oxygen—DO; Apparent Oxygen Utilization—AOU; Export Production—EP; and Calcite saturation state—Ωc). We show that, below the subsurface domains, responses of these drivers are asymmetric and detached from the anthropogenic forcing with large spatial variations. Vast regions of the interior NAtl experience detectable anthropogenic signals significantly earlier and over a longer period than those projected for the near-surface. In contrast to surface domains, the NAtl interior remains largely warmer relative to PI (up to +50%) following the mitigation scenario, with anomalously lower EP, pH, and Ωc (up to −20%) south of 30°N. Oxygen overshoot in the upper mesopelagic of up to +20% is simulated, mainly driven by a decrease in consumption during remineralization. Our study highlights the need for long-term commitment focused on pelagic and deep-water ecosystem monitoring to fully understand the impact of anthropogenic climate change on the North Atlantic biogeochemistry. publishedVersion Article in Journal/Newspaper North Atlantic NORCE vitenarkiv (Norwegian Research Centre) Journal of Geophysical Research: Oceans 127 4
institution Open Polar
collection NORCE vitenarkiv (Norwegian Research Centre)
op_collection_id ftnorce
language English
description Anthropogenic climate change footprints in the ocean go beyond the mixed layer depth, with considerable impacts throughout mesopelagic and deep-ocean ecosystems. Yet, little is known about the timing of these environmental changes, their spatial extent, and the associated timescales of recovery in the ocean interior when strong mitigation strategies are involved. Here, we simulate idealized rapid climate change and mitigation scenarios using the Norwegian Earth System Model to investigate timescales of climate change onset and recovery and the extent of change in the North Atlantic (NAtl) interior relative to Pre-industrial (PI) variability across a suite of environmental drivers (Temperature—Temp; pH; Dissolved Oxygen—DO; Apparent Oxygen Utilization—AOU; Export Production—EP; and Calcite saturation state—Ωc). We show that, below the subsurface domains, responses of these drivers are asymmetric and detached from the anthropogenic forcing with large spatial variations. Vast regions of the interior NAtl experience detectable anthropogenic signals significantly earlier and over a longer period than those projected for the near-surface. In contrast to surface domains, the NAtl interior remains largely warmer relative to PI (up to +50%) following the mitigation scenario, with anomalously lower EP, pH, and Ωc (up to −20%) south of 30°N. Oxygen overshoot in the upper mesopelagic of up to +20% is simulated, mainly driven by a decrease in consumption during remineralization. Our study highlights the need for long-term commitment focused on pelagic and deep-water ecosystem monitoring to fully understand the impact of anthropogenic climate change on the North Atlantic biogeochemistry. publishedVersion
format Article in Journal/Newspaper
author Bertini, Leonardo
Tjiputra, Jerry
spellingShingle Bertini, Leonardo
Tjiputra, Jerry
Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
author_facet Bertini, Leonardo
Tjiputra, Jerry
author_sort Bertini, Leonardo
title Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
title_short Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
title_full Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
title_fullStr Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
title_full_unstemmed Biogeochemical timescales of climate change onset and recovery in the North Atlantic interior under rapid atmospheric CO2 forcing
title_sort biogeochemical timescales of climate change onset and recovery in the north atlantic interior under rapid atmospheric co2 forcing
publishDate 2022
url https://hdl.handle.net/11250/2996935
https://doi.org/10.1029/2021JC017929
genre North Atlantic
genre_facet North Atlantic
op_source Journal of Geophysical Research (JGR): Oceans
127
4
1-22
op_relation Norges forskningsråd: 275268
Norges forskningsråd: 318477
EC/H2020/869357
Journal of Geophysical Research (JGR): Oceans. 2022, 127 (4), 1-22.
urn:issn:2169-9275
https://hdl.handle.net/11250/2996935
https://doi.org/10.1029/2021JC017929
cristin:2021572
op_rights Navngivelse 4.0 Internasjonal
http://creativecommons.org/licenses/by/4.0/deed.no
© 2022, The Authors
op_rightsnorm CC-BY
op_doi https://doi.org/10.1029/2021JC017929
container_title Journal of Geophysical Research: Oceans
container_volume 127
container_issue 4
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