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...

Full description

Bibliographic Details
Main Authors: Bingham, RG, Siegert, MJ, Blankenship, D
Format: Other Non-Article Part of Journal/Newspaper
Language:English
Published: 2005
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