Articles | Volume 15, issue 3
The Cryosphere, 15, 1307–1319, 2021
https://doi.org/10.5194/tc-15-1307-2021
The Cryosphere, 15, 1307–1319, 2021
https://doi.org/10.5194/tc-15-1307-2021

Research article 12 Mar 2021

Research article | 12 Mar 2021

Combined influence of oceanic and atmospheric circulations on Greenland sea ice concentration

Sourav Chatterjee et al.

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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: Reconsider after major revisions (further review by editor and referees) (28 Oct 2020) by Christian Haas
AR by Sourav Chatterjee on behalf of the Authors (09 Dec 2020)  Author's response    Author's tracked changes    Manuscript
ED: Referee Nomination & Report Request started (12 Dec 2020) by Christian Haas
RR by Anonymous Referee #1 (10 Jan 2021)
ED: Publish subject to minor revisions (review by editor) (17 Jan 2021) by Christian Haas
AR by Sourav Chatterjee on behalf of the Authors (25 Jan 2021)  Author's response    Author's tracked changes    Manuscript
ED: Publish as is (30 Jan 2021) by Christian Haas
AR by Sourav Chatterjee on behalf of the Authors (03 Feb 2021)  Author's response    Manuscript
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Short summary
Sea ice in the Greenland Sea (GS) is important for its climatic (fresh water), economical (shipping), and ecological contribution (light availability). The study proposes a mechanism through which sea ice concentration in GS is partly governed by the atmospheric and ocean circulation in the region. The mechanism proposed in this study can be useful for assessing the sea ice variability and its future projection in the GS.