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Climate of the Past An interactive open-access journal of the European Geosciences Union
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Volume 12, issue 3
Clim. Past, 12, 677–695, 2016
https://doi.org/10.5194/cp-12-677-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.
Clim. Past, 12, 677–695, 2016
https://doi.org/10.5194/cp-12-677-2016
© Author(s) 2016. This work is distributed under
the Creative Commons Attribution 3.0 License.

Research article 17 Mar 2016

Research article | 17 Mar 2016

Intra-interglacial climate variability: model simulations of Marine Isotope Stages 1, 5, 11, 13, and 15

Rima Rachmayani et al.

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Reconsider after major revisions (31 Oct 2015) by Martin Claussen
AR by Rima Rachmayani on behalf of the Authors (05 Feb 2016)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Feb 2016) by Martin Claussen
RR by Anonymous Referee #2 (24 Feb 2016)
RR by Anonymous Referee #1 (01 Mar 2016)
ED: Publish subject to minor revisions (review by Editor) (01 Mar 2016) by Martin Claussen
AR by Rima Rachmayani on behalf of the Authors (05 Mar 2016)  Author's response    Manuscript
ED: Publish as is (07 Mar 2016) by Martin Claussen
AR by Rima Rachmayani on behalf of the Authors (08 Mar 2016)  Author's response    Manuscript
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Short summary
A set of 13 interglacial time slice experiments was carried out using a CCSM3-DGVM to study global climate variability between and within the Quaternary interglaciations of MIS 1, 5, 11, 13, and 15. Seasonal surface temperature anomalies can be explained by local insolation anomalies induced by the astronomical forcing in most regions and by GHG forcing at high latitudes and early Bruhnes interglacials. However, climate feedbacks may modify the surface temperature response in specific regions.
A set of 13 interglacial time slice experiments was carried out using a CCSM3-DGVM to study...
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