Basal Melting Along the Floating Part of Byrd Glacier

A mass balance calculation was made for the floating part of Byrd Glacier, using 1978-79 ice elevation and velocity data, over the 45 km of Byrd Glacier from its grounding line to where it leaves its fjord and merges with the Ross Ice Shelf. Smoothed basal melting rates were relatively uniform over...

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Bibliographic Details
Main Authors: Kenneally, James P., Hughes, Terence J.
Format: Text
Language:unknown
Published: DigitalCommons@UMaine 2004
Subjects:
Antarctic Ice Sheet
grounding line
mass balance
Ross Ice Shelf
Earth Sciences
Antarctic
Byrd
Byrd Glacier
Antarc*
Ice Sheet
Ice Shelf
Online Access:https://digitalcommons.library.umaine.edu/ers_facpub/15
https://digitalcommons.library.umaine.edu/cgi/viewcontent.cgi?article=1014&context=ers_facpub
Description
Summary:A mass balance calculation was made for the floating part of Byrd Glacier, using 1978-79 ice elevation and velocity data, over the 45 km of Byrd Glacier from its grounding line to where it leaves its fjord and merges with the Ross Ice Shelf. Smoothed basal melting rates were relatively uniform over this distance and averaged 12 +/- 2 m yr(-1).

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