Fast Flow From the South Pole to Support Force Glacier
The flow of the Antarctic Ice Sheet has for some time been conceptualised as consisting of a small number of fast-flowing ice streams draining relatively stable and inactive interior catchment areas, but recent estimates of surface velocities from synthetic aperture radar interferometry (InSAR) and...
Main Authors: | , , |
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Format: | Other Non-Article Part of Journal/Newspaper |
Language: | English |
Published: |
2005
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Subjects: | |
Online Access: | http://hdl.handle.net/1983/755c10a3-0d50-4935-b32b-9128d0ea9bd0 https://research-information.bris.ac.uk/en/publications/755c10a3-0d50-4935-b32b-9128d0ea9bd0 |