Articles | Volume 14, issue 11
https://doi.org/10.5194/tc-14-4039-2020
https://doi.org/10.5194/tc-14-4039-2020
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, Philippe Huybrechts, Oleg Rybak, and Victor V. Popovnin

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Latest update: 28 Mar 2024
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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.