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Monitoring isostatic rebound in Antarctica with the use of continuous remote GPS observations GPS Solutions, 1999 (Ref: 8408)
Category 1: Peer-reviewed literature

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.

Surface meltstreams on the Amery Ice Shelf, East Antarctica. Annals of Glaciology, 1998 (Ref: 8548)
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Category 1: Peer-reviewed literature

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.

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