Evidence for subglacial water transport in the West Antarctic Ice Sheet through three‐dimensional satellite radar interferometry
- 8 February 2005
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 32 (3)
- https://doi.org/10.1029/2004gl021387
Abstract
No abstract availableKeywords
This publication has 20 references indexed in Scilit:
- Basal Zone of the West Antarctic Ice Streams and its Role in Lubrication of Their Rapid MotionPublished by Wiley ,2013
- Geologic Controls on the Initiation of Rapid Basal Motion for West Antarctic Ice Streams: A Geophysical Perspective Including New Airborne Radar Sounding and Laser Altimetry ResultsPublished by Wiley ,2013
- The West Antarctic Ice Sheet and Sea-Level ChangePublished by Wiley ,2013
- Stabilizing feedbacks in glacier-bed erosionNature, 2003
- An International Plan for Antarctic Subglacial Lake ExplorationPolar Geography, 2003
- Numerical investigations of the slow-down of Whillans Ice Stream, West Antarctica: is it shutting down like Ice Stream C?Annals of Glaciology, 2003
- Velocities and Flux of the Filchner Ice Shelf and its Tributaries Determined from Speckle Tracking InterferometryCanadian Journal of Remote Sensing, 2001
- The onset area of Ice Stream D, West AntarcticaJournal of Glaciology, 2000
- Basal hydraulic system of a West Antarctic ice stream: constraints from borehole observationsJournal of Glaciology, 1997
- A water-piracy hypothesis for the stagnation of Ice Stream C, AntarcticaAnnals of Glaciology, 1994