Persistence and variability of ice-stream grounding lines on retrograde bed slopes
In many ice streams, basal resistance varies in space and time due to the dynamically evolving properties of subglacial till. These variations can cause internally generated oscillations in ice-stream flow. However, the potential for such variations in basal properties is not considered by conventio...
Main Authors: | A. A. Robel, C. Schoof, E. Tziperman |
---|---|
Format: | Article |
Language: | English |
Published: |
Copernicus Publications
2016-08-01
|
Series: | The Cryosphere |
Online Access: | http://www.the-cryosphere.net/10/1883/2016/tc-10-1883-2016.pdf |
Similar Items
-
How dynamic are ice-stream beds?
by: D. Davies, et al.
Published: (2018-05-01) -
Highly variable friction and slip observed at Antarctic ice stream bed
by: Hudson, TS, et al.
Published: (2023) -
The role of subtemperate slip in thermally-driven ice stream margin migration
by: Haseloff, M, et al.
Published: (2018) -
Quantifying bed roughness beneath contemporary and palaeo-ice streams
by: FRANCESCA A.M. FALCINI, et al.
Published: (2018-10-01) -
Tidal bending and strand cracks at the Kamb Ice Stream grounding line, West Antarctica
by: CHRISTINA L. HULBE, et al.
Published: (2016-10-01)