Articles | Volume 13, issue 12
https://doi.org/10.5194/cp-13-1695-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
https://doi.org/10.5194/cp-13-1695-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| Highlight paper
| 
29 Nov 2017
Research article | Highlight paper |
| 29 Nov 2017
Simulation of climate, ice sheets and CO2 evolution during the last four glacial cycles with an Earth system model of intermediate complexity
Andrey Ganopolski
CORRESPONDING AUTHOR
Potsdam Institute for Climate Impact Research (PIK), Potsdam, Germany
Victor Brovkin
Max Plank Institute for Meteorology, Hamburg, Germany
also a guest scientist at: Potsdam Institute for Climate Impact Research (PIK), Potsdam, Germany
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Cited
42 citations as recorded by crossref.
- Interglacials of the Quaternary defined by northern hemispheric land ice distribution outside of Greenland P. Köhler & R. van de Wal 10.1038/s41467-020-18897-5
- Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal M. Willeit et al. 10.1126/sciadv.aav7337
- CO<sub>2</sub> drawdown due to particle ballasting by glacial aeolian dust: an estimate based on the ocean carbon cycle model MPIOM/HAMOCC version 1.6.2p3 M. Heinemann et al. 10.5194/gmd-12-1869-2019
- An oversimplified picture of the climate behavior based on a single process can lead to distorted conclusions R. Lindzen 10.1140/epjp/s13360-020-00471-z
- Mysteriously high Δ<sup>14</sup>C of the glacial atmosphere: influence of <sup>14</sup>C production and carbon cycle changes A. Dinauer et al. 10.5194/cp-16-1159-2020
- Simulating Marine Isotope Stage 7 with a coupled climate–ice sheet model D. Choudhury et al. 10.5194/cp-16-2183-2020
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- Timing and magnitude of Southern Ocean sea ice/carbon cycle feedbacks K. Stein et al. 10.1073/pnas.1908670117
- Anti‐Phased Miocene Ice Volume and CO 2 Changes by Transient Antarctic Ice Sheet Variability L. Stap et al. 10.1029/2020PA003971
- The ultimate cost of carbon D. Archer et al. 10.1007/s10584-020-02785-4
- Reduced-complexity model for the impact of anthropogenic CO<sub>2</sub> emissions on future glacial cycles S. Talento & A. Ganopolski 10.5194/esd-12-1275-2021
- 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
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
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- The Effect of Obliquity-Driven Changes on Paleoclimate Sensitivity During the Late Pleistocene P. Köhler et al. 10.1029/2018GL077717
- Glacial carbon cycle changes by Southern Ocean processes with sedimentary amplification H. Kobayashi et al. 10.1126/sciadv.abg7723
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Modelling the Antarctic Ice Sheet across the mid-Pleistocene transition – implications for Oldest Ice J. Sutter et al. 10.5194/tc-13-2023-2019
- Deglacial Ice Sheet Instabilities Induced by Proglacial Lakes A. Quiquet et al. 10.1029/2020GL092141
- Chaotic and non-chaotic response to quasiperiodic forcing: limits to predictability of ice ages paced by Milankovitch forcing P. Ashwin et al. 10.1093/climsys/dzy002
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- Local oceanic CO<sub>2</sub> outgassing triggered by terrestrial carbon fluxes during deglacial flooding T. Extier et al. 10.5194/cp-18-273-2022
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- Widespread global peatland establishment and persistence over the last 130,000 y C. Treat et al. 10.1073/pnas.1813305116
- The 100 000-Year Periodicity in Glacial Cycles and Oscillations of World Ocean Level V. Bezverkhnii 10.1134/S0001433819040030
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- Machine learning approach reveals strong link between obliquity amplitude increase and the Mid-Brunhes transition T. Mitsui & N. Boers 10.1016/j.quascirev.2021.107344
- Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
- Early Interglacial Legacy of Deglacial Climate Instability S. Barker et al. 10.1029/2019PA003661
- PARASO, a circum-Antarctic fully coupled ice-sheet–ocean–sea-ice–atmosphere–land model involving f.ETISh1.7, NEMO3.6, LIM3.6, COSMO5.0 and CLM4.5 C. Pelletier et al. 10.5194/gmd-15-553-2022
- Antarctic and global climate history viewed from ice cores E. Brook & C. Buizert 10.1038/s41586-018-0172-5
- Observationally Constrained Cloud Phase Unmasks Orbitally Driven Climate Feedbacks N. Sagoo et al. 10.1029/2020GL091873
- Sequential changes in ocean circulation and biological export productivity during the last glacial–interglacial cycle: a model–data study C. O'Neill et al. 10.5194/cp-17-171-2021
42 citations as recorded by crossref.
- Interglacials of the Quaternary defined by northern hemispheric land ice distribution outside of Greenland P. Köhler & R. van de Wal 10.1038/s41467-020-18897-5
- Mid-Pleistocene transition in glacial cycles explained by declining CO 2 and regolith removal M. Willeit et al. 10.1126/sciadv.aav7337
- CO<sub>2</sub> drawdown due to particle ballasting by glacial aeolian dust: an estimate based on the ocean carbon cycle model MPIOM/HAMOCC version 1.6.2p3 M. Heinemann et al. 10.5194/gmd-12-1869-2019
- An oversimplified picture of the climate behavior based on a single process can lead to distorted conclusions R. Lindzen 10.1140/epjp/s13360-020-00471-z
- Mysteriously high Δ<sup>14</sup>C of the glacial atmosphere: influence of <sup>14</sup>C production and carbon cycle changes A. Dinauer et al. 10.5194/cp-16-1159-2020
- Simulating Marine Isotope Stage 7 with a coupled climate–ice sheet model D. Choudhury et al. 10.5194/cp-16-2183-2020
- ChAP 1.0: a stationary tropospheric sulfur cycle for Earth system models of intermediate complexity A. Eliseev et al. 10.5194/gmd-14-7725-2021
- Timing and magnitude of Southern Ocean sea ice/carbon cycle feedbacks K. Stein et al. 10.1073/pnas.1908670117
- Anti‐Phased Miocene Ice Volume and CO 2 Changes by Transient Antarctic Ice Sheet Variability L. Stap et al. 10.1029/2020PA003971
- The ultimate cost of carbon D. Archer et al. 10.1007/s10584-020-02785-4
- Reduced-complexity model for the impact of anthropogenic CO<sub>2</sub> emissions on future glacial cycles S. Talento & A. Ganopolski 10.5194/esd-12-1275-2021
- 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
- On the Cause of the Mid‐Pleistocene Transition C. Berends et al. 10.1029/2020RG000727
- Coupling of a sediment diagenesis model (MEDUSA) and an Earth system model (CESM1.2): a contribution toward enhanced marine biogeochemical modelling and long-term climate simulations T. Kurahashi-Nakamura et al. 10.5194/gmd-13-825-2020
- Back to the Future: Using Long-Term Observational and Paleo-Proxy Reconstructions to Improve Model Projections of Antarctic Climate T. Bracegirdle et al. 10.3390/geosciences9060255
- Extensive introgression at late stages of species formation: Insights from grasshopper hybrid zones L. Hagberg et al. 10.1111/mec.16406
- The Effect of Obliquity-Driven Changes on Paleoclimate Sensitivity During the Late Pleistocene P. Köhler et al. 10.1029/2018GL077717
- Glacial carbon cycle changes by Southern Ocean processes with sedimentary amplification H. Kobayashi et al. 10.1126/sciadv.abg7723
- Low terrestrial carbon storage at the Last Glacial Maximum: constraints from multi-proxy data A. Jeltsch-Thömmes et al. 10.5194/cp-15-849-2019
- Modelling the Antarctic Ice Sheet across the mid-Pleistocene transition – implications for Oldest Ice J. Sutter et al. 10.5194/tc-13-2023-2019
- Deglacial Ice Sheet Instabilities Induced by Proglacial Lakes A. Quiquet et al. 10.1029/2020GL092141
- Chaotic and non-chaotic response to quasiperiodic forcing: limits to predictability of ice ages paced by Milankovitch forcing P. Ashwin et al. 10.1093/climsys/dzy002
- Climate and ice sheet evolutions from the last glacial maximum to the pre-industrial period with an ice-sheet–climate coupled model A. Quiquet et al. 10.5194/cp-17-2179-2021
- Seasonal sea ice persisted through the Holocene Thermal Maximum at 80°N A. Pieńkowski et al. 10.1038/s43247-021-00191-x
- Radiocarbon as a Dating Tool and Tracer in Paleoceanography L. Skinner & E. Bard 10.1029/2020RG000720
- Local oceanic CO<sub>2</sub> outgassing triggered by terrestrial carbon fluxes during deglacial flooding T. Extier et al. 10.5194/cp-18-273-2022
- Last glacial inception trajectories for the Northern Hemisphere from coupled ice and climate modelling T. Bahadory et al. 10.5194/cp-17-397-2021
- 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
- Snapshots of mean ocean temperature over the last 700 000 years using noble gases in the EPICA Dome C ice core M. Haeberli et al. 10.5194/cp-17-843-2021
- Water Mass Versus Sea Level Effects on Benthic Foraminiferal Oxygen Isotope Ratios in the Atlantic Ocean During the LGM R. Völpel et al. 10.1029/2018PA003359
- Widespread global peatland establishment and persistence over the last 130,000 y C. Treat et al. 10.1073/pnas.1813305116
- The 100 000-Year Periodicity in Glacial Cycles and Oscillations of World Ocean Level V. Bezverkhnii 10.1134/S0001433819040030
- Modeling the evolution of pulse-like perturbations in atmospheric carbon and carbon isotopes: the role of weathering–sedimentation imbalances A. Jeltsch-Thömmes & F. Joos 10.5194/cp-16-423-2020
- Late Pleistocene Carbon Cycle Revisited by Considering Solid Earth Processes P. Köhler & G. Munhoven 10.1029/2020PA004020
- Nonlinear climate dynamics: From deterministic behaviour to stochastic excitability and chaos D. Alexandrov et al. 10.1016/j.physrep.2020.11.002
- Machine learning approach reveals strong link between obliquity amplitude increase and the Mid-Brunhes transition T. Mitsui & N. Boers 10.1016/j.quascirev.2021.107344
- Mechanisms of millennial-scale atmospheric CO2 change in numerical model simulations J. Gottschalk et al. 10.1016/j.quascirev.2019.05.013
- Early Interglacial Legacy of Deglacial Climate Instability S. Barker et al. 10.1029/2019PA003661
- PARASO, a circum-Antarctic fully coupled ice-sheet–ocean–sea-ice–atmosphere–land model involving f.ETISh1.7, NEMO3.6, LIM3.6, COSMO5.0 and CLM4.5 C. Pelletier et al. 10.5194/gmd-15-553-2022
- Antarctic and global climate history viewed from ice cores E. Brook & C. Buizert 10.1038/s41586-018-0172-5
- Observationally Constrained Cloud Phase Unmasks Orbitally Driven Climate Feedbacks N. Sagoo et al. 10.1029/2020GL091873
- Sequential changes in ocean circulation and biological export productivity during the last glacial–interglacial cycle: a model–data study C. O'Neill et al. 10.5194/cp-17-171-2021
Latest update: 21 Mar 2023
Short summary
Ice cores reveal that atmospheric CO2 concentration varied synchronously with the global ice volume. Explaining the mechanism of glacial–interglacial variations of atmospheric CO2 concentrations and the link between CO2 and ice sheets evolution still remains a challenge. Here using the Earth system model of intermediate complexity we performed for the first time simulations of co-evolution of climate, ice sheets and carbon cycle using the astronomical forcing as the only external forcing.
Ice cores reveal that atmospheric CO2 concentration varied synchronously with the global ice...
