Tidal motion, ice velocity and melt rate of Petermann Gletscher, Greenland, measured from radar interferometry
Abstract Over a floating glacier ice tongue or an ice shelf, the glacier motion measured by a single, repeat-pass, radar interferogram is difficult to analyze, because the long-term, steady motion of the ice is intermixed with its cyclic, downward motion induced by tidal forcing. Multiple interferog...
Published in: | Journal of Glaciology |
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Format: | Article in Journal/Newspaper |
Language: | English |
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Cambridge University Press (CUP)
1996
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Online Access: | http://dx.doi.org/10.1017/s0022143000003464 https://www.cambridge.org/core/services/aop-cambridge-core/content/view/S0022143000003464 |