Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up

Voermans, Joey J.; Rabault, Jean; Filchuk, Kirill; Ryzhov, Ivan; Heil, Petra; Marchenko, Aleksey; Collins III, Clarence O.; Dabboor, Mohammed; Sutherland, Graig; Babanin, Alexander V.

doi:https://doi.org/10.5194/tc-14-4265-2020

Articles | Volume 14, issue 11

https://doi.org/10.5194/tc-14-4265-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/tc-14-4265-2020

© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 14, issue 11

Research article

|

27 Nov 2020

Research article |

| 27 Nov 2020

Experimental evidence for a universal threshold characterizing wave-induced sea ice break-up

Joey J. Voermans, Jean Rabault, Kirill Filchuk, Ivan Ryzhov, Petra Heil, Aleksey Marchenko, Clarence O. Collins III, Mohammed Dabboor, Graig Sutherland, and Alexander V. Babanin

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Final revised paper (published on 27 Nov 2020)
Preprint (discussion started on 24 Jul 2020)

Interactive discussion

Status: closed

AC: Author comment | RC: Referee comment | SC: Short comment | EC: Editor comment

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- Supplement

RC1: 'Review', Anonymous Referee #1, 01 Sep 2020
- AC1: 'Response to Reviewer 1', Joey Voermans, 30 Sep 2020
RC2: 'review of Voermans et al', Anonymous Referee #2, 24 Sep 2020
- AC2: 'Response to Reviewer 2', Joey Voermans, 30 Sep 2020

Peer-review completion

AR: Author's response | RR: Referee report | ED: Editor decision

ED: Publish subject to minor revisions (review by editor) (05 Oct 2020) by Yevgeny Aksenov

AR by Joey Voermans on behalf of the Authors (07 Oct 2020) Author's response Manuscript

ED: Publish as is (12 Oct 2020) by Yevgeny Aksenov

Short summary

In this work we demonstrate the existence of an observational threshold which identifies when waves are most likely to break sea ice. This threshold is based on information from two recent field campaigns, supplemented with existing observations of sea ice break-up. We show that both field and laboratory observations tend to converge to a single quantitative threshold at which the wave-induced sea ice break-up takes place, which opens a promising avenue for operational forecasting models.