Ice-Bed Coupling Beneath and Beyond Ice Streams: Byrd Glacier, Antarctica

Ice sheet thickness is determined mainly by the strength of ice-bed coupling that controls holistic transitions from slow sheet flow to fast streamflow to buttressing shelf flow. Byrd Glacier has the largest ice drainage system in Antarctica and is the fastest ice stream entering Ross Ice Shelf. In...

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Bibliographic Details
Main Authors: Hughes, Terence J., Sargent, Aitbala, Fastook, James L.
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 2011
Subjects:
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/49
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1048&context=ers_facpub