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We combine ERS-1 satellite radar altimeter surface elevations (Fricker and others, this issue) with six different accumulation distributions to compute balance fluxes for the Lambert Glacier-Amery Ice Shelf Drainage system.
The Lambert Glacier–Amery Ice Shelf system is a major component of the East Antarctic ice sheet. This paper presents two Digital Elevation Models (DEMs) that have been generated for the Lambert Glacier - Amery Ice Shelf system from validated ERS-1 satellite radar altimeter waveform data.
Photometric intensity measurements of the OH(6-2) band P1(2), P1(3), P1(4) and P1(5) emissions were collected at a four minute repetition rate at Davis station, Antarctica during 1994. These data are being examined to determine the magnitude…
A GPS network has been installed to monitor vertical crustal movement … in the Lambert Glacier region, East Antarctica. The program … commenced in January 1998 with a solar-powered GPS system installed at … Beaver Lake.
A solar-powered GPS receiver has been installed near Beaver Lake, Antarctica, to monitor postglacial isostatic rebound that may be occurring as a result of ice thinning near the Lambert glacier since the last glacial maximum.
A topographic map of a 120 km by 20 km section of the Amery Ice Shelf, East Antarctica, mapped with the global positioning system (GPS) in the spring of 1995, revealed two long, shallow troughs in the ice-shelf surface.
A Global Positioning System (GPS) survey has been carried out on the Amery Ice Shelf, providing "ground-truth" measurements of ellipsoidal height for the ERS-1 and ERS-2 satellite altimeters.
Oversnow traverses have collected a variety of glaciological measurements around the interior drainage basin of the Lambert Glacier, East Antarctica (longitudes 54° - 78° E, latitudes 67° - 76S), between 1989-90 and 1994-95.