Articles | Volume 15, issue 5
https://doi.org/10.5194/bg-15-1367-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/bg-15-1367-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
06 Mar 2018
Research article |
| 06 Mar 2018
The influence of the ocean circulation state on ocean carbon storage and CO2 drawdown potential in an Earth system model
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Jonas Nycander
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Kevin I. C. Oliver
National Oceanography Centre, Southampton, University of Southampton, Southampton SO14 3ZH, UK
Laurent Brodeau
Department of Meteorology, Bolin Centre for Climate Research, Stockholm University, 106 91 Stockholm, Sweden
Barcelona Supercomputer Center, Barcelona, Spain
Andy Ridgwell
School of Geographical Sciences, Bristol University, Bristol BS8 1SS, UK
Department of Earth Sciences, University of California-Riverside, Riverside, CA 92521, USA
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Cited
24 citations as recorded by crossref.
- Enhanced vertical mixing in the glacial ocean inferred from sedimentary carbon isotopes S. Wilmes et al. 10.1038/s43247-021-00239-y
- Two‐Timescale Carbon Cycle Response to an AMOC Collapse S. Nielsen et al. 10.1029/2018PA003481
- Carbon Capture and Utilization Technology without Carbon Dioxide Purification and Pressurization: A Review on Its Necessity and Available Technologies H. Ho et al. 10.1021/acs.iecr.9b01213
- Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
- Meridional Ocean Carbon Transport A. Aldama‐Campino et al. 10.1029/2019GB006336
- Paleoredox conditions of bottom water in the northern Indian Ocean since 39 ka R. Nambiar et al. 10.1016/j.palaeo.2021.110766
- Climate pathways behind phytoplankton-induced atmospheric warming R. Asselot et al. 10.5194/bg-19-223-2022
- Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
- Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using <i>δ</i><sup>13</sup>C A. Morée et al. 10.5194/cp-17-753-2021
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- The atmospheric bridge communicated the <i>δ</i><sup>13</sup>C decline during the last deglaciation to the global upper ocean J. Shao et al. 10.5194/cp-17-1507-2021
- Southern Ocean link between changes in atmospheric CO2 levels and northern-hemisphere climate anomalies during the last two glacial periods J. Gottschalk et al. 10.1016/j.quascirev.2019.106067
- Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates K. Kvale et al. 10.1088/1748-9326/aaedc3
- Investigation of Mineral Carbonation with Direct Bubbling into Concrete Sludge M. Abe et al. 10.1021/acsomega.0c04758
- The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
- The devil's in the disequilibrium: multi-component analysis of dissolved carbon and oxygen changes under a broad range of forcings in a general circulation model S. Eggleston & E. Galbraith 10.5194/bg-15-3761-2018
- Global cooling linked to increased glacial carbon storage via changes in Antarctic sea ice A. Marzocchi & M. Jansen 10.1038/s41561-019-0466-8
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- 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
- Linking Glacial‐Interglacial States to Multiple Equilibria of Climate D. Ferreira et al. 10.1029/2018GL077019
- Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle O. Cartapanis et al. 10.5194/cp-14-1819-2018
- Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study H. Zhang et al. 10.1088/2515-7620/aca9ac
- Retracted: Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks P. Vervoort et al. 10.1029/2020PA004090
- The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model R. Asselot et al. 10.1029/2020MS002110
24 citations as recorded by crossref.
- Enhanced vertical mixing in the glacial ocean inferred from sedimentary carbon isotopes S. Wilmes et al. 10.1038/s43247-021-00239-y
- Two‐Timescale Carbon Cycle Response to an AMOC Collapse S. Nielsen et al. 10.1029/2018PA003481
- Carbon Capture and Utilization Technology without Carbon Dioxide Purification and Pressurization: A Review on Its Necessity and Available Technologies H. Ho et al. 10.1021/acs.iecr.9b01213
- Variable C∕P composition of organic production and its effect on ocean carbon storage in glacial-like model simulations M. Ödalen et al. 10.5194/bg-17-2219-2020
- Meridional Ocean Carbon Transport A. Aldama‐Campino et al. 10.1029/2019GB006336
- Paleoredox conditions of bottom water in the northern Indian Ocean since 39 ka R. Nambiar et al. 10.1016/j.palaeo.2021.110766
- Climate pathways behind phytoplankton-induced atmospheric warming R. Asselot et al. 10.5194/bg-19-223-2022
- Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
- Evaluating the biological pump efficiency of the Last Glacial Maximum ocean using <i>δ</i><sup>13</sup>C A. Morée et al. 10.5194/cp-17-753-2021
- Prediction of CO2 solubility in NaCl brine under geological conditions with an improved binary interaction parameter in the Søreide-Whitson model Z. Liu et al. 10.1016/j.geothermics.2022.102544
- The atmospheric bridge communicated the <i>δ</i><sup>13</sup>C decline during the last deglaciation to the global upper ocean J. Shao et al. 10.5194/cp-17-1507-2021
- Southern Ocean link between changes in atmospheric CO2 levels and northern-hemisphere climate anomalies during the last two glacial periods J. Gottschalk et al. 10.1016/j.quascirev.2019.106067
- Asymmetric dynamical ocean responses in warming icehouse and cooling greenhouse climates K. Kvale et al. 10.1088/1748-9326/aaedc3
- Investigation of Mineral Carbonation with Direct Bubbling into Concrete Sludge M. Abe et al. 10.1021/acsomega.0c04758
- The Biological Pump During the Last Glacial Maximum E. Galbraith & L. Skinner 10.1146/annurev-marine-010419-010906
- The devil's in the disequilibrium: multi-component analysis of dissolved carbon and oxygen changes under a broad range of forcings in a general circulation model S. Eggleston & E. Galbraith 10.5194/bg-15-3761-2018
- Global cooling linked to increased glacial carbon storage via changes in Antarctic sea ice A. Marzocchi & M. Jansen 10.1038/s41561-019-0466-8
- Reduced CO2 uptake and growing nutrient sequestration from slowing overturning circulation Y. Liu et al. 10.1038/s41558-022-01555-7
- 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
- Linking Glacial‐Interglacial States to Multiple Equilibria of Climate D. Ferreira et al. 10.1029/2018GL077019
- Carbon burial in deep-sea sediment and implications for oceanic inventories of carbon and alkalinity over the last glacial cycle O. Cartapanis et al. 10.5194/cp-14-1819-2018
- Feedbacks of CaCO3 dissolution effect on ocean carbon sink and seawater acidification: a model study H. Zhang et al. 10.1088/2515-7620/aca9ac
- Retracted: Earth System Model Analysis of How Astronomical Forcing Is Imprinted Onto the Marine Geological Record: The Role of the Inorganic (Carbonate) Carbon Cycle and Feedbacks P. Vervoort et al. 10.1029/2020PA004090
- The Relative Importance of Phytoplankton Light Absorption and Ecosystem Complexity in an Earth System Model R. Asselot et al. 10.1029/2020MS002110
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Short summary
We conclude that different initial states for an ocean model result in different capacities for ocean carbon storage due to differences in the ocean circulation state and the origin of the carbon in the initial ocean carbon reservoir. This could explain why it is difficult to achieve comparable responses of the ocean carbon system in model inter-comparison studies in which the initial states vary between models. We show that this effect of the initial state is quantifiable.
We conclude that different initial states for an ocean model result in different capacities for...
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