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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Volume 12, issue 11
The Cryosphere, 12, 3439-3457, 2018
https://doi.org/10.5194/tc-12-3439-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 12, 3439-3457, 2018
https://doi.org/10.5194/tc-12-3439-2018
© Author(s) 2018. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 01 Nov 2018

Research article | 01 Nov 2018

Ice cliff contribution to the tongue-wide ablation of Changri Nup Glacier, Nepal, central Himalaya

Fanny Brun 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
AR by Fanny Brun on behalf of the Authors (04 Jul 2018)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (08 Jul 2018) by Francesca Pellicciotti
RR by Anonymous Referee #4 (19 Jul 2018)
RR by Anonymous Referee #1 (23 Jul 2018)
ED: Publish subject to minor revisions (review by editor) (03 Sep 2018) by Francesca Pellicciotti
AR by Fanny Brun on behalf of the Authors (06 Sep 2018)  Author's response    Manuscript
ED: Publish subject to technical corrections (30 Sep 2018) by Francesca Pellicciotti
AR by Fanny Brun on behalf of the Authors (12 Oct 2018)  Author's response    Manuscript
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Short summary
On debris-covered glaciers, steep ice cliffs experience dramatically enhanced melt compared with the surrounding debris-covered ice. Using field measurements, UAV data and submetre satellite imagery, we estimate the cliff contribution to 2 years of ablation on a debris-covered tongue in Nepal, carefully taking into account ice dynamics. While they occupy only 7 to 8 % of the tongue surface, ice cliffs contributed to 23 to 24 % of the total tongue ablation.
On debris-covered glaciers, steep ice cliffs experience dramatically enhanced melt compared with...
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