Repeated GPS measurements have been performed at the centre of the Greenlan
d Ice Sheet since 1992. Results have shown that the ice sheet is essentiall
y stable at this location, with GPS-determined strain and elevation change
rates in good accordance with yearly snow accumulation and glaciological fl
ow models. In a local ice cap in East Greenland (Geikie Plateau) repeated G
PS, airborne laser altimetry and SAR interferometry have been used to study
ice movements in the more climatically variable coastal zone, where meter-
level annual elevation changes are possible due to the high precipitation.
The paper outlines the surveys carried out, some preliminary results, and i
ntercomparisons of GPS, laser altimetry and SAR techniques.