Articles | Volume 12, issue 12
https://doi.org/10.5194/cp-12-2195-2016
https://doi.org/10.5194/cp-12-2195-2016
Research article
 | Highlight paper
 | 
15 Dec 2016
Research article | Highlight paper |  | 15 Dec 2016

Last Interglacial climate and sea-level evolution from a coupled ice sheet–climate model

Heiko Goelzer, Philippe Huybrechts, Marie-France Loutre, and Thierry Fichefet

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 (14 Jun 2016) by Denis-Didier Rousseau
AR by Heiko Goelzer on behalf of the Authors (01 Aug 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (11 Aug 2016) by Denis-Didier Rousseau
RR by Anonymous Referee #1 (14 Aug 2016)
RR by Anonymous Referee #2 (23 Aug 2016)
RR by Andrey Ganopolski (05 Sep 2016)
ED: Reconsider after major revisions (06 Sep 2016) by Denis-Didier Rousseau
AR by Heiko Goelzer on behalf of the Authors (10 Oct 2016)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (24 Oct 2016) by Denis-Didier Rousseau
RR by Anonymous Referee #2 (24 Oct 2016)
RR by Anonymous Referee #1 (10 Nov 2016)
ED: Publish subject to technical corrections (10 Nov 2016) by Denis-Didier Rousseau
AR by Heiko Goelzer on behalf of the Authors (11 Nov 2016)  Author's response   Manuscript 
Short summary
We simulate the climate, ice sheet, and sea-level evolution during the Last Interglacial (~ 130 to 115 kyr BP), the most recent warm period in Earth’s history. Our Earth system model includes components representing the atmosphere, the ocean and sea ice, the terrestrial biosphere, and the Greenland and Antarctic ice sheets. Our simulation is in good agreement with available data reconstructions and gives important insights into the dominant mechanisms that caused ice sheet changes in the past.