Articles | Volume 16, issue 3
https://doi.org/10.5194/tc-16-981-2022
https://doi.org/10.5194/tc-16-981-2022
Research article
 | 
14 Mar 2022
Research article |  | 14 Mar 2022

Arctic sea ice anomalies during the MOSAiC winter 2019/20

Klaus Dethloff, Wieslaw Maslowski, Stefan Hendricks, Younjoo J. Lee, Helge F. Goessling, Thomas Krumpen, Christian Haas, Dörthe Handorf, Robert Ricker, Vladimir Bessonov, John J. Cassano, Jaclyn Clement Kinney, Robert Osinski, Markus Rex, Annette Rinke, Julia Sokolova, and Anja Sommerfeld

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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 tc-2020-375', Anonymous Referee #1, 02 Mar 2021
  • RC2: 'Comment on tc-2020-375', Anonymous Referee #2, 31 Mar 2021

Peer review completion

AR: Author's response | RR: Referee report | ED: Editor decision | EF: Editorial file upload
ED: Reconsider after major revisions (further review by editor and referees) (17 Sep 2021) by Petra Heil
AR by Klaus Dethloff on behalf of the Authors (26 Oct 2021)  Author's response   Author's tracked changes   Manuscript 
ED: Referee Nomination & Report Request started (22 Nov 2021) by Petra Heil
RR by Anonymous Referee #1 (04 Dec 2021)
RR by Anonymous Referee #3 (15 Dec 2021)
ED: Publish subject to minor revisions (review by editor) (21 Jan 2022) by Petra Heil
AR by Klaus Dethloff on behalf of the Authors (30 Jan 2022)  Author's response   Author's tracked changes   Manuscript 
ED: Publish as is (13 Feb 2022) by Petra Heil
AR by Klaus Dethloff on behalf of the Authors (14 Feb 2022)  Author's response   Manuscript 
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Short summary
Sea ice thickness anomalies during the MOSAiC (Multidisciplinary drifting Observatory for the Study of Arctic Climate) winter in January, February and March 2020 were simulated with the coupled Regional Arctic climate System Model (RASM) and compared with CryoSat-2/SMOS satellite data. Hindcast and ensemble simulations indicate that the sea ice anomalies are driven by nonlinear interactions between ice growth processes and wind-driven sea-ice transports, with dynamics playing a dominant role.