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The Cryosphere An interactive open-access journal of the European Geosciences Union
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TC | Articles | Volume 14, issue 11
The Cryosphere, 14, 4039–4061, 2020
https://doi.org/10.5194/tc-14-4039-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.
The Cryosphere, 14, 4039–4061, 2020
https://doi.org/10.5194/tc-14-4039-2020
© Author(s) 2020. This work is distributed under
the Creative Commons Attribution 4.0 License.

Research article 16 Nov 2020

Research article | 16 Nov 2020

Modelling the evolution of Djankuat Glacier, North Caucasus, from 1752 until 2100 CE

Yoni Verhaegen 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
ED: Reconsider after major revisions (further review by editor and referees) (13 Jul 2020) by Evgeny A. Podolskiy
AR by Yoni Verhaegen on behalf of the Authors (24 Aug 2020)  Author's response    Manuscript
ED: Referee Nomination & Report Request started (02 Sep 2020) by Evgeny A. Podolskiy
RR by Ann Rowan (11 Sep 2020)
ED: Publish subject to minor revisions (review by editor) (14 Sep 2020) by Evgeny A. Podolskiy
AR by Yoni Verhaegen on behalf of the Authors (19 Sep 2020)  Author's response    Manuscript
ED: Publish as is (28 Sep 2020) by Evgeny A. Podolskiy
Publications Copernicus
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Short summary
We use a numerical flow model to simulate the behaviour of the Djankuat Glacier, a WGMS reference glacier situated in the North Caucasus (Republic of Kabardino-Balkaria, Russian Federation), in response to past, present and future climate conditions (1752–2100 CE). In particular, we adapt a more sophisticated and physically based debris model, which has not been previously applied in time-dependent numerical flow line models, to look at the impact of a debris cover on the glacier’s evolution.
We use a numerical flow model to simulate the behaviour of the Djankuat Glacier, a WGMS...
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