Balance velocity and basal shear stress determinations of an ice stream in West Central Greenland
A theoretical model based on balance velocity and basal shear stress is applied to an ice stream flowing into Jakobshaven Isford glacier Greenland. Balance velocity is defined by Whillans (1977) as a measure of the time change of the mass of a column through the ice thickness. Balance velocities wer...
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Format: | Thesis |
Language: | English |
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The Ohio State University
1978
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Online Access: | http://hdl.handle.net/1811/69221 |