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Climate of the Past An interactive open-access journal of the European Geosciences Union
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We simulate the Last Glacial Maximum atmospheric CO2 decrease with a large ensemble of parameter sets to investigate the range of possible physical and biogeochemical Earth system changes accompanying the CO2 decrease. Amongst the dominant ensemble changes is an increase in terrestrial carbon, which we attribute to a slower soil respiration rate, and the preservation of carbon by the LGM ice sheets. Further investigation into the role of terrestrial carbon is warranted.
CP | Articles | Volume 15, issue 3
Clim. Past, 15, 1039–1062, 2019
https://doi.org/10.5194/cp-15-1039-2019
Clim. Past, 15, 1039–1062, 2019
https://doi.org/10.5194/cp-15-1039-2019

Research article 18 Jun 2019

Research article | 18 Jun 2019

Coupled climate–carbon cycle simulation of the Last Glacial Maximum atmospheric CO2 decrease using a large ensemble of modern plausible parameter sets

Krista M. S. Kemppinen et al.

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Latest update: 15 Jan 2021
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Short summary
We simulate the Last Glacial Maximum atmospheric CO2 decrease with a large ensemble of parameter sets to investigate the range of possible physical and biogeochemical Earth system changes accompanying the CO2 decrease. Amongst the dominant ensemble changes is an increase in terrestrial carbon, which we attribute to a slower soil respiration rate, and the preservation of carbon by the LGM ice sheets. Further investigation into the role of terrestrial carbon is warranted.
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