Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-529-2021
https://doi.org/10.5194/cp-17-529-2021
Research article
 | 
25 Feb 2021
Research article |  | 25 Feb 2021

Mid-Pliocene Atlantic Meridional Overturning Circulation simulated in PlioMIP2

Zhongshi Zhang, Xiangyu Li, Chuncheng Guo, Odd Helge Otterå, Kerim H. Nisancioglu, Ning Tan, Camille Contoux, Gilles Ramstein, Ran Feng, Bette L. Otto-Bliesner, Esther Brady, Deepak Chandan, W. Richard Peltier, Michiel L. J. Baatsen, Anna S. von der Heydt, Julia E. Weiffenbach, Christian Stepanek, Gerrit Lohmann, Qiong Zhang, Qiang Li, Mark A. Chandler, Linda E. Sohl, Alan M. Haywood, Stephen J. Hunter, Julia C. Tindall, Charles Williams, Daniel J. Lunt, Wing-Le Chan, and Ayako Abe-Ouchi

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (24 Nov 2020) by Appy Sluijs
AR by Z.S. Zhang on behalf of the Authors (04 Dec 2020)  Author's response   Manuscript 
ED: Publish as is (14 Jan 2021) by Appy Sluijs
AR by Z.S. Zhang on behalf of the Authors (14 Jan 2021)
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Short summary
The Atlantic Meridional Overturning Circulation (AMOC) is an important topic in the Pliocene Model Intercomparison Project. Previous studies have suggested a much stronger AMOC during the Pliocene than today. However, our current multi-model intercomparison shows large model spreads and model–data discrepancies, which can not support the previous hypothesis. Our study shows good consistency with future projections of the AMOC.