Advanced Search »
Newsletter
Unsubscribe »
National Science Foundation Award #0003616

Studying Byrd Glacier as a Rock-Floored Ice Stream Ending as a Calving Ice Shelf: Phase I

 
Investigator(s): Terence Hughes (PI) ; James Fastook (Co-PI) ; Roger Hooke (Co-PI)
Sponsor: University of Maine, ME 04469 2075811484
Start Date/Expiration Date 2001-02-15 to 2003-01-31 (amended 2001-02-13)
Awarded Amount to Date: $79,787
Abstract: 0003616 Hughes This award supports a one-year study of the floating part of Byrd Glacier, from its grounding line located halfway up a fjord through the Transantarctic Mountains to the end of its lateral rift zone on the Ross Ice Shelf beyond the fjord. Over this l00 km distance, the side boundary changes from rigid between the fjord sidewalls, to nearly free in the lateral rift zone, to deforming when the rifts are healed and Bryd Glacier becomes fully coupled to the Ross Ice Shelf. The stress field for these changing conditions will be calculated a using a gridpoint finite-element model for the Ross Ice Shelf (Thomas and MacAyeal, l982) and a flowband finite-difference model for smooth transitions from sheet flow to stream flow to shelf flow (Hughes, l998). Results of the two modeling approaches will be compared, using existing ice elevation and velocity data obtained from aerial photogrammetry, our unpublished surface mass balance data, and new velocity data obtained from Landsat imagery by the U. S. Geological Survey. This study will train one graduate student at the Masters level.
NSF Org: ANT - Antarctic Sciences Section
Award Number: 0003616
Award Instrument: Standard Grant
Program Manager: Julie Palais
ANT Antarctic Sciences Section
OPP Office of Polar Programs
NSF Program(s): ANTARCTIC GLACIOLOGY, EXP PROG TO STIM COMP RES
Field Application(s): Polar Programs-Related
Program Reference Code(s): EXP PROG TO STIM COMP RES, 9150
UNASSIGNED, 0000
Program Element Code(s): 5116
EXP PROG TO STIM COMP RES, 9150