Articles | Volume 17, issue 4
https://doi.org/10.5194/tc-17-1445-2023
https://doi.org/10.5194/tc-17-1445-2023
Research article
 | 
04 Apr 2023
Research article |  | 04 Apr 2023

Rapid sea ice changes in the future Barents Sea

Ole Rieke, Marius Årthun, and Jakob Simon Dörr

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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 egusphere-2022-324', Anonymous Referee #1, 11 Jul 2022
    • AC1: 'Reply on RC1', Ole Rieke, 27 Sep 2022
  • RC2: 'Comment on egusphere-2022-324', Anonymous Referee #2, 01 Sep 2022
    • AC2: 'Reply on RC2', Ole Rieke, 27 Sep 2022

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Publish subject to revisions (further review by editor and referees) (14 Oct 2022) by Jari Haapala
AR by Ole Rieke on behalf of the Authors (24 Oct 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish subject to revisions (further review by editor and referees) (15 Nov 2022) by Jari Haapala
ED: Referee Nomination & Report Request started (28 Dec 2022) by Jari Haapala
RR by Anonymous Referee #1 (19 Jan 2023)
RR by Anonymous Referee #2 (15 Feb 2023)
ED: Publish subject to technical corrections (03 Mar 2023) by Jari Haapala
AR by Ole Rieke on behalf of the Authors (10 Mar 2023)  Author's response   Manuscript 
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Short summary
The Barents Sea is the region of most intense winter sea ice loss, and future projections show a continued decline towards ice-free conditions by the end of this century but with large fluctuations. Here we use climate model simulations to look at the occurrence and drivers of rapid ice change events in the Barents Sea that are much stronger than the average ice loss. A better understanding of these events will contribute to improved sea ice predictions in the Barents Sea.