Articles | Volume 9, issue 6
The Cryosphere, 9, 2383–2398, 2015
https://doi.org/10.5194/tc-9-2383-2015
The Cryosphere, 9, 2383–2398, 2015
https://doi.org/10.5194/tc-9-2383-2015

Research article 15 Dec 2015

Research article | 15 Dec 2015

Summertime evolution of snow specific surface area close to the surface on the Antarctic Plateau

Q. Libois et al.

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AR: Author's response | RR: Referee report | ED: Editor decision
AR by Q. Libois on behalf of the Authors (17 Nov 2015)  Author's response    Manuscript
ED: Publish subject to minor revisions (Editor review) (27 Nov 2015) by Martin Schneebeli
AR by Q. Libois on behalf of the Authors (27 Nov 2015)  Author's response    Manuscript
ED: Publish as is (02 Dec 2015) by Martin Schneebeli
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Short summary
The albedo and surface energy budget of the Antarctic Plateau are largely determined by snow specific surface area. The latter experiences substantial daily-to-seasonal variations in response to meteorological conditions. In particular, it decreases by a factor three in summer, causing a drop in albedo. These variations are monitored from in situ and remote sensing observations at Dome C. For the first time, they are also simulated with a snowpack evolution model adapted to Antarctic conditions.