Elevation change measurements of the Greenland Ice Sheet

7Citations
Citations of this article
17Readers
Mendeley users who have this article in their library.

Abstract

Repeated GPS measurements have been performed at the centre of the Greenland Ice Sheet since 1992. Results have shown that the ice sheet is essentially stable at this location, with GPS-determined strain and elevation change rates in good accordance with yearly snow accumulation and glaciological flow models. In a local ice cap in East Greenland (Geikie Plateau) repeated GPS, 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 intercomparisons of GPS, laser altimetry and SAR techniques. © 2000, The Seismological Society of Japan, Society of Geomagnetism and Earth, Planetary and Space Sciences, The Volcanological Society of Japan, The Geodetic Society of Japan, The Japanese Society for Planetary Sciences. All rights reserved.

Cite

CITATION STYLE

APA

Forsberg, R., Keller, K., Nielsen, C. S., Gundestrup, N., Tscherning, C. C., Madsen, S. N., & Dall, J. (2000). Elevation change measurements of the Greenland Ice Sheet. Earth, Planets and Space, 52(11), 1049–1053. https://doi.org/10.1186/BF03352329

Register to see more suggestions

Mendeley helps you to discover research relevant for your work.

Already have an account?

Save time finding and organizing research with Mendeley

Sign up for free