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
In spite of significant progress in paleoclimate reconstructions and modelling of different aspects of the past glacial cycles, the mechanisms which transform regional and seasonal variations in solar insolation into long-term and global-scale glacial–interglacial cycles are still not f...
| Main Authors: | , |
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| Format: | Article |
| Language: | English |
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Copernicus Publications
2017-11-01
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| Series: | Climate of the Past |
| Online Access: | https://www.clim-past.net/13/1695/2017/cp-13-1695-2017.pdf |
| _version_ | 1818581524475281408 |
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| author | A. Ganopolski V. Brovkin V. Brovkin |
| author_facet | A. Ganopolski V. Brovkin V. Brovkin |
| author_sort | A. Ganopolski |
| collection | DOAJ |
| description | In spite of significant progress in paleoclimate reconstructions and modelling
of different aspects of the past glacial cycles, the mechanisms which
transform regional and seasonal variations in solar insolation into long-term
and global-scale glacial–interglacial cycles are still not fully understood – in particular, in relation to CO<sub>2</sub> variability. Here using the Earth system model of intermediate complexity CLIMBER-2 we performed simulations of the co-evolution of climate, ice sheets, and carbon cycle over the last 400 000 years using the orbital forcing as the only external forcing. The model simulates temporal dynamics of CO<sub>2</sub>, global ice volume, and other climate system characteristics in good agreement with paleoclimate reconstructions. These results provide strong support for the idea that long and strongly asymmetric glacial cycles of the late Quaternary represent a direct but strongly nonlinear response of the Northern Hemisphere ice sheets to orbital forcing. This response is strongly amplified and globalised by the carbon cycle feedbacks. Using simulations performed with the model in different configurations, we also analyse the role of individual processes and sensitivity to the choice of model parameters. While many features of simulated glacial cycles are rather robust, some details of CO<sub>2</sub>
evolution, especially during glacial terminations, are sensitive to the
choice of model parameters. Specifically, we found two major regimes of
CO<sub>2</sub> changes during terminations: in the first one, when the recovery of the Atlantic meridional overturning circulation (AMOC) occurs only at the end
of the termination, a pronounced overshoot in CO<sub>2</sub> concentration occurs at the beginning of the interglacial and CO<sub>2</sub> remains almost constant during the interglacial or even declines towards the end, resembling Eemian CO<sub>2</sub> dynamics. However, if the recovery of the AMOC occurs in the middle of the glacial termination, CO<sub>2</sub> concentration continues to rise during the interglacial, similar to the Holocene. We also discuss the potential contribution of the brine rejection mechanism for the CO<sub>2</sub> and carbon isotopes in the atmosphere and the ocean during the past glacial termination. |
| first_indexed | 2024-12-16T07:34:52Z |
| format | Article |
| id | doaj.art-c4e4ba57c74b4ac5935e073971b0d5ac |
| institution | Directory Open Access Journal |
| issn | 1814-9324 1814-9332 |
| language | English |
| last_indexed | 2024-12-16T07:34:52Z |
| publishDate | 2017-11-01 |
| publisher | Copernicus Publications |
| record_format | Article |
| series | Climate of the Past |
| spelling | doaj.art-c4e4ba57c74b4ac5935e073971b0d5ac2022-12-21T22:39:16ZengCopernicus PublicationsClimate of the Past1814-93241814-93322017-11-01131695171610.5194/cp-13-1695-2017Simulation of climate, ice sheets and CO<sub>2</sub> evolution during the last four glacial cycles with an Earth system model of intermediate complexityA. Ganopolski0V. Brovkin1V. Brovkin2Potsdam Institute for Climate Impact Research (PIK), Potsdam, GermanyMax Plank Institute for Meteorology, Hamburg, Germanyalso a guest scientist at: Potsdam Institute for Climate Impact Research (PIK), Potsdam, GermanyIn spite of significant progress in paleoclimate reconstructions and modelling of different aspects of the past glacial cycles, the mechanisms which transform regional and seasonal variations in solar insolation into long-term and global-scale glacial–interglacial cycles are still not fully understood – in particular, in relation to CO<sub>2</sub> variability. Here using the Earth system model of intermediate complexity CLIMBER-2 we performed simulations of the co-evolution of climate, ice sheets, and carbon cycle over the last 400 000 years using the orbital forcing as the only external forcing. The model simulates temporal dynamics of CO<sub>2</sub>, global ice volume, and other climate system characteristics in good agreement with paleoclimate reconstructions. These results provide strong support for the idea that long and strongly asymmetric glacial cycles of the late Quaternary represent a direct but strongly nonlinear response of the Northern Hemisphere ice sheets to orbital forcing. This response is strongly amplified and globalised by the carbon cycle feedbacks. Using simulations performed with the model in different configurations, we also analyse the role of individual processes and sensitivity to the choice of model parameters. While many features of simulated glacial cycles are rather robust, some details of CO<sub>2</sub> evolution, especially during glacial terminations, are sensitive to the choice of model parameters. Specifically, we found two major regimes of CO<sub>2</sub> changes during terminations: in the first one, when the recovery of the Atlantic meridional overturning circulation (AMOC) occurs only at the end of the termination, a pronounced overshoot in CO<sub>2</sub> concentration occurs at the beginning of the interglacial and CO<sub>2</sub> remains almost constant during the interglacial or even declines towards the end, resembling Eemian CO<sub>2</sub> dynamics. However, if the recovery of the AMOC occurs in the middle of the glacial termination, CO<sub>2</sub> concentration continues to rise during the interglacial, similar to the Holocene. We also discuss the potential contribution of the brine rejection mechanism for the CO<sub>2</sub> and carbon isotopes in the atmosphere and the ocean during the past glacial termination.https://www.clim-past.net/13/1695/2017/cp-13-1695-2017.pdf |
| spellingShingle | A. Ganopolski V. Brovkin V. Brovkin 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 Climate of the Past |
| title | 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 |
| title_full | 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 |
| title_fullStr | 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 |
| title_full_unstemmed | 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 |
| title_short | 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 |
| title_sort | 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 |
| url | https://www.clim-past.net/13/1695/2017/cp-13-1695-2017.pdf |
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