Articles | Volume 15, issue 13
https://doi.org/10.5194/bg-15-4163-2018
© Author(s) 2018. 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-15-4163-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
the Creative Commons Attribution 4.0 License.
Research article
| 
10 Jul 2018
Research article |
| 10 Jul 2018
| 10 Jul 2018
Long-term response of oceanic carbon uptake to global warming via physical and biological pumps
Atmospheric an Ocean Research Institute, University of Tokyo,
Kashiwa, Japan
Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
Ayako Abe-Ouchi
Atmospheric an Ocean Research Institute, University of Tokyo,
Kashiwa, Japan
Japan Agency for Marine-Earth Science and Technology (JAMSTEC), Yokohama, Japan
Yasuhiro Yamanaka
Graduate School of Environmental Science, Hokkaido University,
Sapporo, Japan
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- Multi‐Century Changes in the Ocean Carbon Cycle Controlled by the Tropical Oceans and the Southern Ocean M. Chikamoto & P. DiNezio 10.1029/2021GB007090
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- Responses of marine ecosystems to climate change impacts and their treatment in biogeochemical ecosystem models C. Ani & B. Robson 10.1016/j.marpolbul.2021.112223
- A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al. 10.1029/2021PA004302
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22 citations as recorded by crossref.
- Scaling and intermittent properties of oceanic and atmospheric pCO2 time series and their difference in a turbulence framework K. Robache et al. 10.5194/npg-32-35-2025
- Crucial Role of Bacterial Processes in the Net Community Production of the Amundsen Sea Polynya Disclosed by a Modeling Study Y. Kwon et al. 10.1029/2023JG007718
- Carbon Export in the Ocean: A Biologist's Perspective M. Iversen 10.1146/annurev-marine-032122-035153
- Competing and accelerating effects of anthropogenic nutrient inputs on climate-driven changes in ocean carbon and oxygen cycles A. Yamamoto et al. 10.1126/sciadv.abl9207
- Development of the MIROC-ES2L Earth system model and the evaluation of biogeochemical processes and feedbacks T. Hajima et al. 10.5194/gmd-13-2197-2020
- Ocean carbon pump decomposition and its application to CMIP5 earth system model simulations A. Oka 10.1186/s40645-020-00338-y
- Cycling Rates of Particulate Organic Carbon Along the GEOTRACES Pacific Meridional Transect GP15 V. Amaral et al. 10.1029/2023GB007940
- Climate change impacts on sea-ice ecosystems and associated ecosystem services N. Steiner et al. 10.1525/elementa.2021.00007
- Warming of newly-subducted subtropical mode water in the North Pacific was suppressed from 1999 to 2017 X. Zhang & F. Xu 10.1088/1748-9326/ad97d0
- Multi‐Century Changes in the Ocean Carbon Cycle Controlled by the Tropical Oceans and the Southern Ocean M. Chikamoto & P. DiNezio 10.1029/2021GB007090
- Glacial CO2 decrease and deep-water deoxygenation by iron fertilization from glaciogenic dust A. Yamamoto et al. 10.5194/cp-15-981-2019
- Responses of marine ecosystems to climate change impacts and their treatment in biogeochemical ecosystem models C. Ani & B. Robson 10.1016/j.marpolbul.2021.112223
- A First Intercomparison of the Simulated LGM Carbon Results Within PMIP‐Carbon: Role of the Ocean Boundary Conditions F. Lhardy et al. 10.1029/2021PA004302
- Quantifying biological carbon pump pathways with a data-constrained mechanistic model ensemble approach M. Stukel et al. 10.5194/bg-19-3595-2022
- Clarifying the role of inorganic carbon in blue carbon policy and practice W. Turrell et al. 10.1016/j.marpol.2023.105873
- Seasonal Variability and Estimation of Annual East Siberian Sea Phytoplankton Primary Production and Comparison with the Other Siberian Seas A. Demidov et al. 10.1134/S0001437020050045
- Evaluation of Ocean Biogeochemistry and Carbon Cycling in CMIP Earth System Models With the International Ocean Model Benchmarking (IOMB) Software System W. Fu et al. 10.1029/2022JC018965
- 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
- Calibration of temperature-dependent ocean microbial processes in the cGENIE.muffin (v0.9.13) Earth system model K. Crichton et al. 10.5194/gmd-14-125-2021
- The climatology of the deep particle flux in the oligotrophic western North Atlantic gyre, 1978–2022 M. Conte et al. 10.1016/j.pocean.2025.103433
- Millennium time-scale experiments on climate-carbon cycle with doubled CO2 concentration T. Hajima et al. 10.1186/s40645-020-00350-2
- Sensitivity of atmospheric CO2 to regional variability in particulate organic matter remineralization depths J. Wilson et al. 10.5194/bg-16-2923-2019
Discussed (final revised paper)
Latest update: 01 Jul 2025
Short summary
Millennial-scale changes in oceanic CO2 uptake due to global warming are simulated by a GCM and offline biogeochemical model. Sensitivity studies show that decreases in oceanic CO2 uptake are mainly caused by a weaker biological pump and seawater warming. Enhanced CO2 uptake due to weaker equatorial upwelling cancels out reduced CO2 uptake due to weaker AMOC and AABW formation. Thus, circulation change plays only a small direct role in reduction of CO2 uptake due to global warming.
Millennial-scale changes in oceanic CO2 uptake due to global warming are simulated by a GCM and...
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