Influence of the surface moraine on the state of Djankuat Glacier (Central Caucasus) by 2025
Current glaciation of the Central Caucasus is in the regressive stage of evolution. Observed long rising of the air temperature in the ablation seasons (almost 1 °C since 1968 on the Djankuat Glacier) together with insignificant growth of winter precipitation caused a long period of the glacier degr...
| Main Authors: | , |
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| Format: | Article |
| Language: | Russian |
| Published: |
Nauka
2018-09-01
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| Series: | Лëд и снег |
| Subjects: | |
| Online Access: | https://ice-snow.igras.ru/jour/article/view/482 |