Radio Echo Sounding on a Valley Glacier in East Greenland

Abstract Although radio echo sounding equipment has been used with success for measuring the thickness of ice sheets in the Arctic and Antarctic, a valley glacier poses the additional problems of echoes from the valley walls, which may obscure the bottom echoes, and a high attenuation of radio waves...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Davis, J. L., Halliday, J. S., Miller, K. J.
Format: Article in Journal/Newspaper
Language:English
Published: Cambridge University Press (CUP) 1973
Subjects:
Online Access:http://dx.doi.org/10.1017/s0022143000022723
https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000022723
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Summary:Abstract Although radio echo sounding equipment has been used with success for measuring the thickness of ice sheets in the Arctic and Antarctic, a valley glacier poses the additional problems of echoes from the valley walls, which may obscure the bottom echoes, and a high attenuation of radio waves in the ice. During July and August 1970, a study was carried out on Roslin Gletscher in Stauning Alper, East Greenland, to investigate the problems of radio echo sounding on a valley glacier. Results show that reflections from the valley walls are minimized by using sufficiently directional antennae, but attenuation of the signal in the ice is higher than that in polar ice at the same temperature. Water in and on the ice probably accounts for much of the attenuation, and the use of a lower frequency or measurements before the melt commences should give improved performance.