Investigating the local-scale influence of sea ice on Greenland surface melt

Stroeve, Julienne C.; Mioduszewski, John R.; Rennermalm, Asa; Boisvert, Linette N.; Tedesco, Marco; Robinson, David

doi:https://doi.org/10.5194/tc-11-2363-2017

Articles | Volume 11, issue 5

https://doi.org/10.5194/tc-11-2363-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Special issue:

Mass balance of the Greenland Ice Sheet

https://doi.org/10.5194/tc-11-2363-2017

© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Articles | Volume 11, issue 5

Special issue editorial

|

23 Oct 2017

Special issue editorial |

| 23 Oct 2017

Investigating the local-scale influence of sea ice on Greenland surface melt

Julienne C. Stroeve, John R. Mioduszewski, Asa Rennermalm, Linette N. Boisvert, Marco Tedesco, and David Robinson

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Final revised paper (published on 23 Oct 2017)
Preprint (discussion started on 05 May 2017)

Interactive discussion

Status: closed

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

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SC1: 'Minor reference clarification', Jeremy Fyke, 20 May 2017
- AC1: 'Fyfe comments', Julienne Stroeve, 21 May 2017
RC1: 'Review Comments', Anonymous Referee #1, 05 Jun 2017
RC2: 'Review of "Investigating the Local Scale Influence of Sea Ice on Greenland Surface Melt" by J.C. Stroeve et al.', Anonymous Referee #2, 04 Jul 2017

Peer-review completion

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

AR by Anna Mirena Feist-Polner on behalf of the Authors (10 Aug 2017) Author's response Manuscript

ED: Publish as is (14 Aug 2017) by Edward Hanna

Short summary

As the sea ice has declined strongly in recent years there has been a corresponding increase in Greenland melting. While both are likely a result of changes in atmospheric circulation patterns that favor summer melt, this study evaluates whether or not sea ice reductions around the Greenland ice sheet are having an influence on Greenland summer melt through enhanced sensible and latent heat transport from open water areas onto the ice sheet.