Adaptively constraining radar attenuation and temperature across the Thwaites Glacier catchment using bed echoes
ABSTRACT Englacial temperature is a major control on ice rheology and flow. However, it is difficult to measure at the glacier to ice-sheet scale. As a result, ice-sheet models must make assumptions about englacial temperature and rheology, which affect sea level projections. This is problematic if...
| Published in: | Journal of Glaciology |
|---|---|
| Main Authors: | , , , |
| Format: | Article in Journal/Newspaper |
| Language: | English |
| Published: |
Cambridge University Press (CUP)
2016
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| Subjects: | |
| Online Access: | http://dx.doi.org/10.1017/jog.2016.100 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143016001003 |