Tidal motion, ice velocity and melt rate of Petermann Gletscher, Greenland, measured from radar interferometry
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 interferograms and...
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
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eScholarship, University of California
1996
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| Online Access: | https://escholarship.org/uc/item/36d8b95c |