Articles | Volume 13, issue 7
https://doi.org/10.5194/cp-13-959-2017
https://doi.org/10.5194/cp-13-959-2017
Research article
 | 
27 Jul 2017
Research article |  | 27 Jul 2017

Antarctic climate and ice-sheet configuration during the early Pliocene interglacial at 4.23 Ma

Nicholas R. Golledge, Zoë A. Thomas, Richard H. Levy, Edward G. W. Gasson, Timothy R. Naish, Robert M. McKay, Douglas E. Kowalewski, and Christopher J. Fogwill

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 (18 Mar 2017) by Zhengtang Guo
AR by Nicholas Golledge on behalf of the Authors (11 Apr 2017)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (24 Apr 2017) by Zhengtang Guo
RR by Anonymous Referee #2 (12 May 2017)
RR by Anonymous Referee #1 (16 May 2017)
ED: Publish as is (06 Jun 2017) by Zhengtang Guo
Download
Short summary
We investigated how the Antarctic climate and ice sheets evolved during a period of warmer-than-present temperatures 4 million years ago, during a time when the carbon dioxide concentration in the atmosphere was very similar to today's level. Using computer models to first simulate the climate, and then how the ice sheets responded, we found that Antarctica most likely lost around 8.5  m sea-level equivalent ice volume as both East and West Antarctic ice sheets retreated.