Articles | Volume 14, issue 10
https://doi.org/10.5194/tc-14-3329-2020
https://doi.org/10.5194/tc-14-3329-2020
Research article
 | 
06 Oct 2020
Research article |  | 06 Oct 2020

Frazil ice growth and production during katabatic wind events in the Ross Sea, Antarctica

Lisa Thompson, Madison Smith, Jim Thomson, Sharon Stammerjohn, Steve Ackley, and Brice Loose

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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
ED: Publish subject to minor revisions (review by editor) (17 Jun 2020) by Olaf Eisen
AR by Brice Loose on behalf of the Authors (23 Jun 2020)  Author's response   Manuscript 
ED: Publish subject to minor revisions (review by editor) (08 Jul 2020) by Olaf Eisen
AR by Brice Loose on behalf of the Authors (21 Jul 2020)
ED: Publish as is (02 Aug 2020) by Olaf Eisen
AR by Brice Loose on behalf of the Authors (11 Aug 2020)  Manuscript 
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Short summary
The offshore winds around Antarctica can reach hurricane strength and produce intense cooling, causing the surface ocean to form a slurry of seawater and ice crystals. For the first time, we observed a buildup of heat and salt in the surface ocean, caused by loose ice crystal formation. We conclude that up to 1 m of ice was formed per day by the intense cooling, suggesting that unconsolidated crystals may be an important part of the total freezing that happens around Antarctica.