Articles | Volume 20, issue 4
https://doi.org/10.5194/cp-20-1067-2024
https://doi.org/10.5194/cp-20-1067-2024
Research article
 | 
02 May 2024
Research article |  | 02 May 2024

Highly stratified mid-Pliocene Southern Ocean in PlioMIP2

Julia E. Weiffenbach, Henk A. Dijkstra, Anna S. von der Heydt, Ayako Abe-Ouchi, Wing-Le Chan, Deepak Chandan, Ran Feng, Alan M. Haywood, Stephen J. Hunter, Xiangyu Li, Bette L. Otto-Bliesner, W. Richard Peltier, Christian Stepanek, Ning Tan, Julia C. Tindall, and Zhongshi Zhang

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Review of cp-2023-83', Anonymous Referee #1, 14 Dec 2023
  • RC2: 'Review on cp-2023-83', Chris Brierley, 20 Dec 2023

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to minor revisions (review by editor) (09 Feb 2024) by Alessio Rovere
AR by Julia Weiffenbach on behalf of the Authors (19 Feb 2024)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (01 Mar 2024) by Alessio Rovere
AR by Julia Weiffenbach on behalf of the Authors (04 Mar 2024)
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Short summary
Elevated atmospheric CO2 concentrations and a smaller Antarctic Ice Sheet during the mid-Pliocene (~ 3 million years ago) cause the Southern Ocean surface to become fresher and warmer, which affects the global ocean circulation. The CO2 concentration and the smaller Antarctic Ice Sheet both have a similar and approximately equal impact on the Southern Ocean. The conditions of the Southern Ocean in the mid-Pliocene could therefore be analogous to those in a future climate with smaller ice sheets.