Evidence for a Frozen Bed, Byrd Glacier, Antarctica

Ice thickness, computed within the fjord region of Byrd Glacier on the assumptions that Byrd Glacier is in mass-balance equilibrium and that ice velocity is entirely due to basal sliding, are on average 400 m less than measured ice thicknesses along a radio-echo profile. We consider four explanation...

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Bibliographic Details
Main Authors: Scofield, John P., Fastook, James L., Hughes, Terence J.
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 1991
Subjects:
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/32
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1031&context=ers_facpub