Articles | Volume 11, issue 3
The Cryosphere, 11, 1035–1040, 2017
The Cryosphere, 11, 1035–1040, 2017

Brief communication 03 May 2017

Brief communication | 03 May 2017

Brief communication: Impacts of ocean-wave-induced breakup of Antarctic sea ice via thermodynamics in a stand-alone version of the CICE sea-ice model

Luke G. Bennetts et al.


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 Luke Bennetts on behalf of the Authors (17 Mar 2017)  Author's response    Manuscript
ED: Publish subject to technical corrections (31 Mar 2017) by Dirk Notz
Short summary
A numerical model is used to investigate how Antarctic sea ice concentration and volume are affected by increased melting caused by ocean-wave breakup of the ice. When temperatures are high enough to melt the ice, concentration and volume are reduced for ~ 100 km into the ice-covered ocean. When temperatures are low enough for ice growth, the concentration recovers, but the reduced volume persists.