Search of Fall Meeting 1998 database
1998 Fall Meeting
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HR: 0830h
AN: G41D-03
TI: Surface Morphology of the Central West Antarctic Ice Sheet From
Airborne Laser Altimetry
AU: Blankenship, D D
EM: blank@ig.utexas.edu
AF: Institute for Geophysics
The University of Texas at Austin
4412 Spicewood Springs Rd #600 Austin, Tx 78759-8500
AU: Bell, R E
EM: robinb@ldeo.columbia.edu
AF: Lamont Doherty Earth Observatory
Torrey Cliff Palisades, NY 10964-8000
AU: *Morse, D L
EM: morse@ig.utexas.edu
AF: Institute for Geophysics
The University of Texas at Austin
4412 Spicewood Springs Rd #600 Austin, Tx 78759-8500
AU: Kempf, S D
EM: scottk@ig.utexas.edu
AF: Institute for Geophysics
The University of Texas at Austin
4412 Spicewood Springs Rd #600 Austin, Tx 78759-8500
AU: Arko, R B
EM: arko@ldeo.columbia.edu
AF: Lamont Doherty Earth Observatory
Torrey Cliff Palisades, NY 10964-8000
AU: Guillemot, C J
EM: chrisg@unavco.ucar.edu
AF: UNAVCO/UCAR
P.O. Box 3000
Boulder, Co 80307-3000
AU: Brozena, J M
EM: john@hp8c.nrl.navy.mil
AF: Naval Research Laboratory
455 Overlook Ave
Washington, DC
AU: Jarvis, J L
EM: I:jim@nrl.navy.mil
AF: Naval Research Laboratory
455 Overlook Ave
Washington, DC
AU: Childers, V A
EM:
AF: Naval Research Laboratory
455 Overlook Ave
Washington, DC
AU: Hodge, S M
EM: smhodge@usgs.gov
AF: Naval Research Laboratory
455 Overlook Ave
Washington, DC
AU: Hodge, S M
EM: smhodge@usgs.gov
AF: USGS
Ice Dynamics Project Office
University of Puget Sound
119 Thompson Hall Tacoma, Wa 98416
AU: Scambos, T A
EM: teds@icehouse.colorado.edu
AF: National Snow and Ice Data Center
CIRES Campus Box 449; 1540 30th St.
University of Colorado
Boulder, Co 80309-0449
AB: The portion of the West Antarctic ice sheet (WAIS)
encompassing the ice divide separating the Pine Island and
Ross Embayments and the initiation of ice streams B, C and D
within the Ross Embayment is an increasing focus for WAIS
research. Proposed activities include both deep ice coring
and shallow coring traverses near the divide as well as
seismological traverses of the ice stream onsets. Here we
report on results of the laser altimetry component of two
aerogeophysical surveys of this region: the first is a
50,000 line-km survey collected by the CASERTZ (Corridor
Aerogeophysics of the Interior Ross Embayment) project on a
5.3 km grid over the onsets of ice streams B and C; the
second is a 100,000 line-km survey (also on a 5.3 km grid)
collected by the Support Office for Aerogeophysical Research
(SOAR) covering ice stream D from the ice divide to the
grounding line.
Both of these surveys utilized a 900 W (peak-power) pulsed
laser (23 nsec pulse at 1064 nm) with a 3.5 m footprint (at
a flight elevation of 500 m). The average range from the
aircraft to the ice surface was determined every eight to
nine meters along the flight path by summing the
travel-times for 64 laser returns. These averaged laser
ranges were ultimately projected to a position on the ice
surface using aircraft attitude information from an on-board
laser gyroscope. The aircraft position was determined
kinematically using differential carrier phase GPS
observations made at one-second intervals with multiple
receivers. Surface elevations determined with this system
have single-season uncorrected mean deviations for
observations made at points of intersecting flight paths
ranging from 0.13 to 1.3 meters. These mean deviations are
reduced to 0.09 m to .37 m after correcting profiles for a
linear drift in the vertical position of the aircraft.
These new surface elevation data provide a calibration
surface for space-based altimetry measurements and are a
benchmark for future ice sheet volume change detection.
Augmented by satellite imagery, these data also should be
sufficient for resolving the position of the topographic ice
divide and boundaries of ice stream initiation with the
sub-kilometer precision necessary for modeling WAIS
dynamics.
DE: 9310 Antarctica
DE: 1827 Glaciology (1863)
DE: 1640 Remote sensing
SC: G
MN: 1998 Fall Meeting
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