Articles | Volume 17, issue 1
https://doi.org/10.5194/cp-17-37-2021
https://doi.org/10.5194/cp-17-37-2021
Research article
 | 
11 Jan 2021
Research article |  | 11 Jan 2021

A multi-model CMIP6-PMIP4 study of Arctic sea ice at 127 ka: sea ice data compilation and model differences

Masa Kageyama, Louise C. Sime, Marie Sicard, Maria-Vittoria Guarino, Anne de Vernal, Ruediger Stein, David Schroeder, Irene Malmierca-Vallet, Ayako Abe-Ouchi, Cecilia Bitz, Pascale Braconnot, Esther C. Brady, Jian Cao, Matthew A. Chamberlain, Danny Feltham, Chuncheng Guo, Allegra N. LeGrande, Gerrit Lohmann, Katrin J. Meissner, Laurie Menviel, Polina Morozova, Kerim H. Nisancioglu, Bette L. Otto-Bliesner, Ryouta O'ishi, Silvana Ramos Buarque, David Salas y Melia, Sam Sherriff-Tadano, Julienne Stroeve, Xiaoxu Shi, Bo Sun, Robert A. Tomas, Evgeny Volodin, Nicholas K. H. Yeung, Qiong Zhang, Zhongshi Zhang, Weipeng Zheng, and Tilo Ziehn

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Status: closed
Status: closed
AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment
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Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision
ED: Publish subject to minor revisions (review by editor) (18 May 2020) by Marie-France Loutre
AR by Masa Kageyama on behalf of the Authors (08 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (19 Jun 2020) by Marie-France Loutre
AR by Masa Kageyama on behalf of the Authors (14 Aug 2020)  Author's response   Manuscript 
ED: Publish subject to technical corrections (07 Sep 2020) by Marie-France Loutre
AR by Masa Kageyama on behalf of the Authors (06 Oct 2020)  Author's response   Manuscript 

Post-review adjustments

AA: Author's adjustment | EA: Editor approval
AA by Masa Kageyama on behalf of the Authors (02 Dec 2020)   Author's adjustment   Manuscript
EA: Adjustments approved (04 Dec 2020) by Marie-France Loutre
Short summary
The Last interglacial (ca. 127 000 years ago) is a period with increased summer insolation at high northern latitudes, resulting in a strong reduction in Arctic sea ice. The latest PMIP4-CMIP6 models all simulate this decrease, consistent with reconstructions. However, neither the models nor the reconstructions agree on the possibility of a seasonally ice-free Arctic. Work to clarify the reasons for this model divergence and the conflicting interpretations of the records will thus be needed.