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The Cryosphere An interactive open-access journal of the European Geosciences Union
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Volume 11, issue 1
The Cryosphere, 11, 133–138, 2017
https://doi.org/10.5194/tc-11-133-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.
The Cryosphere, 11, 133–138, 2017
https://doi.org/10.5194/tc-11-133-2017
© Author(s) 2017. This work is distributed under
the Creative Commons Attribution 3.0 License.

Brief communication 18 Jan 2017

Brief communication | 18 Jan 2017

Brief communication: Thinning of debris-covered and debris-free glaciers in a warming climate

Argha Banerjee

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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
AR by Argha Banerjee on behalf of the Authors (23 Sep 2016)  Author's response    Manuscript
ED: Reconsider after major revisions (29 Sep 2016) by G. Hilmar Gudmundsson
ED: Referee Nomination & Report Request started (27 Oct 2016) by G. Hilmar Gudmundsson
RR by Anonymous Referee #2 (15 Nov 2016)
RR by Anonymous Referee #3 (27 Nov 2016)
ED: Publish subject to minor revisions (Editor review) (11 Dec 2016) by G. Hilmar Gudmundsson
AR by Argha Banerjee on behalf of the Authors (20 Dec 2016)  Author's response    Manuscript
ED: Publish as is (25 Dec 2016) by G. Hilmar Gudmundsson
Publications Copernicus
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Short summary
Measurements of debris-covered and debris-free glaciers in the Himalaya-Karakoram show similar decadal scale thinning, despite a suppression of melt under the debris. Using physical arguments, supported by simulations of 1-D idealised glaciers, we analyse the evolution of thinning rates on both glacier types under a warming climate. The dynamics of the emergence velocity profile control the thinning rate evolution in general and lead to the observed trends in the thinning rate data.
Measurements of debris-covered and debris-free glaciers in the Himalaya-Karakoram show similar...
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