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The Cryosphere An interactive open-access journal of the European Geosciences Union
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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.
TC | Articles | Volume 14, issue 11
The Cryosphere, 14, 4039–4061, 2020
https://doi.org/10.5194/tc-14-4039-2020
The Cryosphere, 14, 4039–4061, 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 et al.

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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.
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