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...
Published in: | Journal of Geophysical Research: Oceans |
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Online Access: | https://hdl.handle.net/11250/2996935 https://doi.org/10.1029/2021JC017929 |
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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 |
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Open Polar |
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NORCE vitenarkiv (Norwegian Research Centre) |
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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 |
_version_ |
1766123220100972544 |