Articles | Volume 17, issue 5
https://doi.org/10.5194/cp-17-1919-2021
https://doi.org/10.5194/cp-17-1919-2021
Research article
 | 
28 Sep 2021
Research article |  | 28 Sep 2021

Does a difference in ice sheets between Marine Isotope Stages 3 and 5a affect the duration of stadials? Implications from hosing experiments

Sam Sherriff-Tadano, Ayako Abe-Ouchi, Akira Oka, Takahito Mitsui, and Fuyuki Saito

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Interactive discussion

Status: closed

Comment types: AC – author | RC – referee | CC – community | EC – editor | CEC – chief editor | : Report abuse
  • RC1: 'Comment on cp-2021-47', Anonymous Referee #1, 31 May 2021
  • RC2: 'Comment on cp-2021-47', Anonymous Referee #2, 17 Jun 2021

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) (29 Jul 2021) by Laurie Menviel
AR by Sam Sherriff-Tadano on behalf of the Authors (18 Aug 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to technical corrections (26 Aug 2021) by Laurie Menviel
AR by Sam Sherriff-Tadano on behalf of the Authors (31 Aug 2021)  Author's response   Manuscript 
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Short summary
Glacial periods underwent climate shifts between warm states and cold states on a millennial timescale. Frequency of these climate shifts varied along time: it was shorter during mid-glacial period compared to early glacial period. Here, from climate simulations of early and mid-glacial periods with a comprehensive climate model, we show that the larger ice sheet in the mid-glacial compared to early glacial periods could contribute to the frequent climate shifts during the mid-glacial period.