Articles | Volume 18, issue 10
https://doi.org/10.5194/bg-18-3189-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/bg-18-3189-2021
© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Ocean carbon cycle feedbacks in CMIP6 models: contributions from different basins
Anna Katavouta
CORRESPONDING AUTHOR
Department of Earth, Ocean and Ecological Sciences, School of Environmental Sciences, University of Liverpool, Liverpool, UK
National Oceanography Centre, Liverpool, UK
Richard G. Williams
Department of Earth, Ocean and Ecological Sciences, School of Environmental Sciences, University of Liverpool, Liverpool, UK
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Cited
15 citations as recorded by crossref.
- Biogeochemical Timescales of Climate Change Onset and Recovery in the North Atlantic Interior Under Rapid Atmospheric CO2 Forcing L. Bertini & J. Tjiputra 10.1029/2021JC017929
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- Diagnosing CO2 emission-induced feedbacks between the Southern Ocean carbon cycle and the climate system: A multiple Earth System Model analysis using a water mass tracking approach T. Roy et al. 10.1175/JCLI-D-20-0889.1
- Asymmetries in the Southern Ocean contribution to global heat and carbon uptake R. Williams et al. 10.1038/s41558-024-02066-3
- A weakened AMOC may prolong greenhouse gas–induced Mediterranean drying even with significant and rapid climate change mitigation T. Delworth et al. 10.1073/pnas.2116655119
- Response of atmospheric pCO$$_2$$ to a strong AMOC weakening under low and high emission scenarios A. Boot et al. 10.1007/s00382-024-07295-y
- Modulation of regional carbon uptake by AMOC and alkalinity changes in the subpolar North Atlantic under a warming climate Q. Zhang et al. 10.3389/fmars.2024.1304193
- Weakening AMOC reduces ocean carbon uptake and increases the social cost of carbon F. Schaumann & E. Alastrué de Asenjo 10.1073/pnas.2419543122
- No compromise in efficiency from the co-application of a marine and a terrestrial CDR method Y. Moustakis et al. 10.1038/s41467-025-59982-x
- Scenario choice impacts carbon allocation projection at global warming levels L. de Mora et al. 10.5194/esd-14-1295-2023
- Stronger Oceanic CO2 Sink in Eddy‐Resolving Simulations of Global Warming D. Couespel et al. 10.1029/2023GL106172
- The Southern Ocean Carbon Cycle 1985–2018: Mean, Seasonal Cycle, Trends, and Storage J. Hauck et al. 10.1029/2023GB007848
- What goes in must come out: the oceanic outgassing of anthropogenic carbon D. Couespel & J. Tjiputra 10.1088/1748-9326/ad16e0
- The role of the Southern Ocean in the global climate response to carbon emissions R. Williams et al. 10.1098/rsta.2022.0062
- Hydrological cycle amplification imposes spatial patterns on the climate change response of ocean pH and carbonate chemistry A. Hogikyan & L. Resplandy 10.5194/bg-21-4621-2024
15 citations as recorded by crossref.
- Biogeochemical Timescales of Climate Change Onset and Recovery in the North Atlantic Interior Under Rapid Atmospheric CO2 Forcing L. Bertini & J. Tjiputra 10.1029/2021JC017929
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- Diagnosing CO2 emission-induced feedbacks between the Southern Ocean carbon cycle and the climate system: A multiple Earth System Model analysis using a water mass tracking approach T. Roy et al. 10.1175/JCLI-D-20-0889.1
- Asymmetries in the Southern Ocean contribution to global heat and carbon uptake R. Williams et al. 10.1038/s41558-024-02066-3
- A weakened AMOC may prolong greenhouse gas–induced Mediterranean drying even with significant and rapid climate change mitigation T. Delworth et al. 10.1073/pnas.2116655119
- Response of atmospheric pCO$$_2$$ to a strong AMOC weakening under low and high emission scenarios A. Boot et al. 10.1007/s00382-024-07295-y
- Modulation of regional carbon uptake by AMOC and alkalinity changes in the subpolar North Atlantic under a warming climate Q. Zhang et al. 10.3389/fmars.2024.1304193
- Weakening AMOC reduces ocean carbon uptake and increases the social cost of carbon F. Schaumann & E. Alastrué de Asenjo 10.1073/pnas.2419543122
- No compromise in efficiency from the co-application of a marine and a terrestrial CDR method Y. Moustakis et al. 10.1038/s41467-025-59982-x
- Scenario choice impacts carbon allocation projection at global warming levels L. de Mora et al. 10.5194/esd-14-1295-2023
- Stronger Oceanic CO2 Sink in Eddy‐Resolving Simulations of Global Warming D. Couespel et al. 10.1029/2023GL106172
- The Southern Ocean Carbon Cycle 1985–2018: Mean, Seasonal Cycle, Trends, and Storage J. Hauck et al. 10.1029/2023GB007848
- What goes in must come out: the oceanic outgassing of anthropogenic carbon D. Couespel & J. Tjiputra 10.1088/1748-9326/ad16e0
- The role of the Southern Ocean in the global climate response to carbon emissions R. Williams et al. 10.1098/rsta.2022.0062
- Hydrological cycle amplification imposes spatial patterns on the climate change response of ocean pH and carbonate chemistry A. Hogikyan & L. Resplandy 10.5194/bg-21-4621-2024
Latest update: 21 May 2025
Short summary
Diagnostics of the latest-generation Earth system models reveal the ocean will continue to absorb a large fraction of the anthropogenic carbon released to the atmosphere in the next century, with the Atlantic Ocean storing a large amount of this carbon relative to its size. The ability of the ocean to absorb carbon will reduce in the future as the ocean warms and acidifies. This reduction is larger in the Atlantic Ocean due to a weakening of the meridional overturning with changes in climate.
Diagnostics of the latest-generation Earth system models reveal the ocean will continue to...
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