Articles | Volume 14, issue 2
Geosci. Model Dev., 14, 1101–1124, 2021
https://doi.org/10.5194/gmd-14-1101-2021
Geosci. Model Dev., 14, 1101–1124, 2021
https://doi.org/10.5194/gmd-14-1101-2021

Development and technical paper 24 Feb 2021

Development and technical paper | 24 Feb 2021

A fully coupled Arctic sea-ice–ocean–atmosphere model (ArcIOAM v1.0) based on C-Coupler2: model description and preliminary results

Shihe Ren et al.

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Interactive discussion

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
AR by Shihe Ren on behalf of the Authors (12 Nov 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (13 Nov 2020) by Alexander Robel
RR by David Bailey (18 Nov 2020)
ED: Reconsider after major revisions (24 Nov 2020) by Alexander Robel
AR by Shihe Ren on behalf of the Authors (02 Jan 2021)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (06 Jan 2021) by Alexander Robel
RR by David Bailey (19 Jan 2021)
ED: Publish subject to technical corrections (20 Jan 2021) by Alexander Robel
AR by Shihe Ren on behalf of the Authors (23 Jan 2021)  Author's response    Manuscript
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Short summary
Sea ice plays a crucial role in global energy and water budgets. To get a better simulation of sea ice, we coupled a sea ice model with an atmospheric and ocean model to form a fully coupled system. The sea ice simulation results of this coupled system demonstrated that a two-way coupled model has better performance in terms of sea ice, especially in summer. This indicates that sea-ice–ocean–atmosphere interaction plays a crucial role in controlling Arctic summertime sea ice distribution.