Study of characteristics of the supraglacial runoff of the Austre Grønfjordbreen, Spitsbergen
Surface runoff on the glacier is represented by two aquifers: a hydro-network of streams and a porous layer of melting crust in which meltwater moves. The first one transfers water from the snowmelt zone, and the second one drains the ablation area. Data on the state of the melting crust at various...
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| Format: | Article |
| Language: | Russian |
| Published: |
Nauka
2023-04-01
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| Series: | Лëд и снег |
| Subjects: | |
| Online Access: | https://ice-snow.igras.ru/jour/article/view/1150 |
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