Timing of stagnation of Ice Stream C, West Antarctica, from short-pulse radar studies of buried surface crevasses
Five short-pulse radar profiles were run across the edge of inactive Ice Stream C, one of the “Ross” ice streams that flows from the West Antarctic inland ice sheet into the Ross Ice Shelf. Scatter from buried crevasses, which we presume were at the surface of the ice stream when it was active, crea...
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| Veröffentlicht in: | Journal of glaciology 1993, Vol.39 (133), p.553-561 |
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| Hauptverfasser: | , |
| Format: | Artikel |
| Sprache: | eng |
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