Unsteady flow inferred for Thwaites Glacier, and comparison with Pine Island Glacier, West Antarctica
We present a comparison of surface velocities in 1996, derived from interferometric synthetic aperture radar, with an estimate of the long-term, depth-averaged velocity based on the assumption of steady-state flow for both Pine Island Glacier and its neighbour, Thwaites Glacier, West Antarctica. The...
| Main Authors: | , |
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| Format: | Article in Journal/Newspaper |
| Language: | unknown |
| Published: |
eScholarship, University of California
2002
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| Subjects: | |
| Online Access: | https://escholarship.org/uc/item/1p17h4rz |