Articles | Volume 12, issue 3
https://doi.org/10.5194/cp-12-677-2016
https://doi.org/10.5194/cp-12-677-2016
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, Matthias Prange, and Michael Schulz

Download

Interactive discussion

Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
Printer-friendly Version - Printer-friendly version Supplement - Supplement

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
Download
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.