Earth System Dynamics
Earth System Dynamics
ESD
Articles | Volume 9, issue 2
Articles | Volume 9, issue 2
https://doi.org/10.5194/esd-9-413-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
https://doi.org/10.5194/esd-9-413-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
Articles | Volume 9, issue 2
Research article
 | 
25 Apr 2018
Research article |  | 25 Apr 2018

Earth system model simulations show different feedback strengths of the terrestrial carbon cycle under glacial and interglacial conditions

Markus Adloff, Christian H. Reick, and Martin Claussen

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Latest update: 10 Dec 2024
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Short summary
Computer simulations show that during an ice age a strong atmospheric CO2 increase would have resulted in stronger carbon uptake of the continents than today. Causes are the larger potential of glacial vegetation to increase its photosynthetic efficiency under increasing CO2 and the smaller amount of carbon in extratropical soils during an ice age that can be released under greenhouse warming. Hence, for different climates the Earth system is differently sensitive to carbon cycle perturbations.
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