Faster decline and higher variability in the sea ice thickness of the marginal Arctic seas when accounting for dynamic snow cover

Mallett, Robbie D. C.; Stroeve, Julienne C.; Tsamados, Michel; Landy, Jack C.; Willatt, Rosemary; Nandan, Vishnu; Liston, Glen E.

doi:https://doi.org/10.5194/tc-15-2429-2021

Articles | Volume 15, issue 5

https://doi.org/10.5194/tc-15-2429-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

https://doi.org/10.5194/tc-15-2429-2021

© Author(s) 2021. This work is distributed under
the Creative Commons Attribution 4.0 License.

Articles | Volume 15, issue 5

Research article

| Highlight paper

|

04 Jun 2021

Research article | Highlight paper |

| 04 Jun 2021

Faster decline and higher variability in the sea ice thickness of the marginal Arctic seas when accounting for dynamic snow cover

Robbie D. C. Mallett, Julienne C. Stroeve, Michel Tsamados, Jack C. Landy, Rosemary Willatt, Vishnu Nandan, and Glen E. Liston

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Final revised paper (published on 04 Jun 2021)
Supplement to the final revised paper
Preprint (discussion started on 28 Oct 2020)
Supplement to the preprint

Interactive discussion

Status: closed

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

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- Supplement

RC1: 'Review of tc-2020-282 Faster decline and higher variability in the sea ice thickness of the marginal Arctic seas', Stefan Kern, 23 Nov 2020
- AC2: 'Reply on RC1', Robbie Mallett, 05 Feb 2021
RC2: 'Review of manuscript', Anonymous Referee #2, 13 Dec 2020
- AC1: 'Reply on RC2', Robbie Mallett, 05 Feb 2021

Peer-review completion

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

ED: Publish subject to revisions (further review by editor and referees) (23 Feb 2021) by Ruth Mottram

AR by Robbie Mallett on behalf of the Authors (09 Mar 2021) Author's response Author's tracked changes Manuscript

ED: Publish as is (31 Mar 2021) by Ruth Mottram

Short summary

We re-estimate pan-Arctic sea ice thickness (SIT) values by combining data from the Envisat and CryoSat-2 missions with data from a new, reanalysis-driven snow model. Because a decreasing amount of ice is being hidden below the waterline by the weight of overlying snow, we argue that SIT may be declining faster than previously calculated in some regions. Because the snow product varies from year to year, our new SIT calculations also display much more year-to-year variability.