Articles | Volume 12, issue 12
https://doi.org/10.5194/cp-12-2145-2016
© Author(s) 2016. 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-12-2145-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
the Creative Commons Attribution 3.0 License.
Research article
| 
29 Nov 2016
Research article |
| 29 Nov 2016
Modelled interglacial carbon cycle dynamics during the Holocene, the Eemian and Marine Isotope Stage (MIS) 11
Thomas Kleinen
CORRESPONDING AUTHOR
Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg,
Germany
Victor Brovkin
Max Planck Institute for Meteorology, Bundesstr. 53, 20146 Hamburg,
Germany
Guy Munhoven
LPAP, Institut d'Astrophysique et de Géophysique, Université
de Liège, Liège, Belgium
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Cited
22 citations as recorded by crossref.
- Impact of terrestrial biosphere on the atmospheric CO<sub>2</sub> concentration across Termination V G. Hes et al. 10.5194/cp-18-1429-2022
- The influence of orbital parameters on the North American Monsoon system during the Last Interglacial Period N. Insel & M. Berkelhammer 10.1002/jqs.3311
- Extensive loss of past permafrost carbon but a net accumulation into present-day soils A. Lindgren et al. 10.1038/s41586-018-0371-0
- Use of the Gas Emission Site Type Method in the Evaluation of the CO2 Emissions in Raised Bogs R. Cieśliński & K. Kubiak-Wójcicka 10.3390/w16071069
- Widespread global peatland establishment and persistence over the last 130,000 y C. Treat et al. 10.1073/pnas.1813305116
- What was the source of the atmospheric CO<sub>2</sub> increase during the Holocene? V. Brovkin et al. 10.5194/bg-16-2543-2019
- Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
- Atmospheric methane underestimated in future climate projections T. Kleinen et al. 10.1088/1748-9326/ac1814
- Strong increase in thawing of subsea permafrost in the 22nd century caused by anthropogenic climate change S. Wilkenskjeld et al. 10.5194/tc-16-1057-2022
- Human Impact on Water Circulation Patterns in Raised Bogs of the Baltic Type, Northern Poland Z. Lipińska et al. 10.3390/su151612277
- Ocean carbon inventory under warmer climate conditions – the case of the Last Interglacial A. Kessler et al. 10.5194/cp-14-1961-2018
- Global vegetation distribution driving factors in two Dynamic Global Vegetation Models of contrasting complexities H. Li et al. 10.1016/j.gloplacha.2019.05.009
- Wetter Summers Mitigated Temperature Stress on Rocky Mountain Forests During the Last Interglacial Warm Period M. Berkelhammer et al. 10.1029/2021GL093678
- Simulation of climate, ice sheets and CO<sub>2</sub> evolution during the last four glacial cycles with an Earth system model of intermediate complexity A. Ganopolski & V. Brovkin 10.5194/cp-13-1695-2017
- Pollen and macrofossil‐inferred palaeoclimate at the Ridge Site, Hudson Bay Lowlands, Canada: evidence for a dry climate and significant recession of the Laurentide Ice Sheet during Marine Isotope Stage 3 A. Dalton et al. 10.1111/bor.12218
- Late Pleistocene chronology, palaeoecology and stratigraphy at a suite of sites along the Albany River, Hudson Bay Lowlands, Canada A. Dalton et al. 10.1016/j.palaeo.2017.12.011
- Late Holocene climate: Natural or anthropogenic? W. Ruddiman et al. 10.1002/2015RG000503
- Comparative carbon cycle dynamics of the present and last interglacial V. Brovkin et al. 10.1016/j.quascirev.2016.01.028
- Sundaland Peat Carbon Dynamics and Its Contribution to the Holocene Atmospheric CO2 Concentration J. Abrams et al. 10.1002/2017GB005763
- Insights and issues with estimating northern peatland carbon stocks and fluxes since the Last Glacial Maximum J. Loisel et al. 10.1016/j.earscirev.2016.12.001
- Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
- Constraining the Late Pleistocene history of the Laurentide Ice Sheet by dating the Missinaibi Formation, Hudson Bay Lowlands, Canada A. Dalton et al. 10.1016/j.quascirev.2016.06.015
14 citations as recorded by crossref.
- Impact of terrestrial biosphere on the atmospheric CO<sub>2</sub> concentration across Termination V G. Hes et al. 10.5194/cp-18-1429-2022
- The influence of orbital parameters on the North American Monsoon system during the Last Interglacial Period N. Insel & M. Berkelhammer 10.1002/jqs.3311
- Extensive loss of past permafrost carbon but a net accumulation into present-day soils A. Lindgren et al. 10.1038/s41586-018-0371-0
- Use of the Gas Emission Site Type Method in the Evaluation of the CO2 Emissions in Raised Bogs R. Cieśliński & K. Kubiak-Wójcicka 10.3390/w16071069
- Widespread global peatland establishment and persistence over the last 130,000 y C. Treat et al. 10.1073/pnas.1813305116
- What was the source of the atmospheric CO<sub>2</sub> increase during the Holocene? V. Brovkin et al. 10.5194/bg-16-2543-2019
- Marine Isotope Stage 11c: An unusual interglacial P. Tzedakis et al. 10.1016/j.quascirev.2022.107493
- Atmospheric methane underestimated in future climate projections T. Kleinen et al. 10.1088/1748-9326/ac1814
- Strong increase in thawing of subsea permafrost in the 22nd century caused by anthropogenic climate change S. Wilkenskjeld et al. 10.5194/tc-16-1057-2022
- Human Impact on Water Circulation Patterns in Raised Bogs of the Baltic Type, Northern Poland Z. Lipińska et al. 10.3390/su151612277
- Ocean carbon inventory under warmer climate conditions – the case of the Last Interglacial A. Kessler et al. 10.5194/cp-14-1961-2018
- Global vegetation distribution driving factors in two Dynamic Global Vegetation Models of contrasting complexities H. Li et al. 10.1016/j.gloplacha.2019.05.009
- Wetter Summers Mitigated Temperature Stress on Rocky Mountain Forests During the Last Interglacial Warm Period M. Berkelhammer et al. 10.1029/2021GL093678
- Simulation of climate, ice sheets and CO<sub>2</sub> evolution during the last four glacial cycles with an Earth system model of intermediate complexity A. Ganopolski & V. Brovkin 10.5194/cp-13-1695-2017
8 citations as recorded by crossref.
- Pollen and macrofossil‐inferred palaeoclimate at the Ridge Site, Hudson Bay Lowlands, Canada: evidence for a dry climate and significant recession of the Laurentide Ice Sheet during Marine Isotope Stage 3 A. Dalton et al. 10.1111/bor.12218
- Late Pleistocene chronology, palaeoecology and stratigraphy at a suite of sites along the Albany River, Hudson Bay Lowlands, Canada A. Dalton et al. 10.1016/j.palaeo.2017.12.011
- Late Holocene climate: Natural or anthropogenic? W. Ruddiman et al. 10.1002/2015RG000503
- Comparative carbon cycle dynamics of the present and last interglacial V. Brovkin et al. 10.1016/j.quascirev.2016.01.028
- Sundaland Peat Carbon Dynamics and Its Contribution to the Holocene Atmospheric CO2 Concentration J. Abrams et al. 10.1002/2017GB005763
- Insights and issues with estimating northern peatland carbon stocks and fluxes since the Last Glacial Maximum J. Loisel et al. 10.1016/j.earscirev.2016.12.001
- Understanding the causes and consequences of past marine carbon cycling variability through models D. Hülse et al. 10.1016/j.earscirev.2017.06.004
- Constraining the Late Pleistocene history of the Laurentide Ice Sheet by dating the Missinaibi Formation, Hudson Bay Lowlands, Canada A. Dalton et al. 10.1016/j.quascirev.2016.06.015
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Short summary
We investigate trends in atmospheric CO2 during three recent interglacials – the Holocene, the Eemian and MIS 11 – using an earth system model of intermediate complexity. Our model experiments show a considerable improvement in the modelled CO2 trends for all three interglacials if peat accumulation and shallow water CaCO3 sedimentation are included, forcing the model only with orbital and sea level changes. The Holocene CO2 trend requires anthropogenic emissions of CO2 only after 3 ka BP.
We investigate trends in atmospheric CO2 during three recent interglacials – the Holocene, the...
