Articles | Volume 12, issue 12
https://doi.org/10.5194/cp-12-2145-2016
https://doi.org/10.5194/cp-12-2145-2016
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, Victor Brovkin, and Guy Munhoven

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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (17 Jul 2015) by Luke Skinner
AR by Thomas Kleinen on behalf of the Authors (14 Oct 2016)
ED: Publish subject to technical corrections (18 Oct 2016) by Luke Skinner
AR by Thomas Kleinen on behalf of the Authors (24 Oct 2016)  Author's response   Manuscript 
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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.