A further comparison of glacier velocities measured by radio-echo and survey methods

A comparison has been mager between ice velocities that were measured by the radio-echo technique and by a survey method on the Devon Island ice cap, Arctic Canada (lat. 75° 23' N., long. 82° 23'W.). Results were 2.58±0.11 ma1 by radar and 2.17±0.20 m a–1 by survey. The discrepancy between...

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Bibliographic Details
Published in:Journal of Glaciology
Main Authors: Doake, C.S.M., Gorman, M., Paterson, W.S.B.
Format: Article in Journal/Newspaper
Language:unknown
Published: International Glaciological Society 1976
Subjects:
Online Access:http://nora.nerc.ac.uk/id/eprint/525647/
https://doi.org/10.3189/S0022143000030690
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Summary:A comparison has been mager between ice velocities that were measured by the radio-echo technique and by a survey method on the Devon Island ice cap, Arctic Canada (lat. 75° 23' N., long. 82° 23'W.). Results were 2.58±0.11 ma1 by radar and 2.17±0.20 m a–1 by survey. The discrepancy between the two measurements is within the limits of statistical significance, and the methods are consigerred to give comparable results.