The thermal structure of the Recovery Glacier drainage basin, Antarctica, derived from three-dimensional numerical flow modelling
The basal conditions of the ice sheet are of crucial importance for the dynamics of the ice, as they determine the sliding at the ice base. Since the base is hardly accessible for in situ observations, indirect measurements of the basal properties are of great interest. The bed reflectivity derived...
| Main Authors: | , , |
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| Format: | Conference Object |
| Language: | unknown |
| Published: |
2015
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| Subjects: | |
| Online Access: | https://epic.awi.de/id/eprint/42743/ https://www.igsoc.org/symposia/2015/cambridge/proceedings/proceedings.html https://hdl.handle.net/10013/epic.49350 |