Articles | Volume 13, issue 10
https://doi.org/10.5194/tc-13-2597-2019
https://doi.org/10.5194/tc-13-2597-2019
Research article
 | 
07 Oct 2019
Research article |  | 07 Oct 2019

The surface albedo of the Greenland Ice Sheet between 1982 and 2015 from the CLARA-A2 dataset and its relationship to the ice sheet's surface mass balance

Aku Riihelä, Michalea D. King, and Kati Anttila

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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: Reconsider after major revisions (29 Jun 2019) by Mark Flanner
AR by Aku Riihelä on behalf of the Authors (02 Jul 2019)  Author's response   Manuscript 
ED: Referee Nomination & Report Request started (10 Jul 2019) by Mark Flanner
RR by Jason Box (18 Jul 2019)
RR by Anonymous Referee #1 (29 Aug 2019)
ED: Publish subject to minor revisions (review by editor) (30 Aug 2019) by Mark Flanner
AR by Aku Riihelä on behalf of the Authors (04 Sep 2019)  Author's response   Manuscript 
ED: Publish as is (05 Sep 2019) by Mark Flanner
AR by Aku Riihelä on behalf of the Authors (09 Sep 2019)
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Short summary
We used a 1982–2015 time series of satellite observations to examine changes in surface reflectivity (albedo) of the Greenland Ice Sheet. We found notable decreases in albedo over most of the ice sheet margins in July and August, particularly over the west coast and between 2000 and 2015. The results indicate that significant melt now occurs in areas 50 to 100 m higher up the ice sheet relative to the early 1980s. The albedo decrease is consistent and covarying with modelled ice sheet mass loss.