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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DigitalCommons@UMaine
2011
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Online Access: | https://digitalcommons.library.umaine.edu/ers_facpub/49 https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1048&context=ers_facpub |