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Hydraulic run-away: a mechanism for thermally regulated surges of ice sheets
A. C. Fowler
, C. Johnson
University of Oxford
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Earth and Planetary Sciences
Ice Sheet
100%
Ice Stream
100%
Valley Glacier
50%
Feedback
50%
Water Pressure
50%
Ross Ice Shelf
50%
Water Storage
50%
Drainage Basin
50%
Ice Thickness
50%
Strait
50%