Evidence for a recently abandoned shear margin adjacent to ice stream B2, Antarctica, from ice‐penetrating radar measurements
Open Access
- 10 June 2000
- journal article
- research article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 105 (B6) , 13409-13422
- https://doi.org/10.1029/2000jb900037
Abstract
No abstract availableKeywords
This publication has 66 references indexed in Scilit:
- Changes in the margin of Ice Stream C, AntarcticaJournal of Glaciology, 2000
- Tributaries of West Antarctic Ice Streams Revealed by RADARSAT InterferometryScience, 1999
- Thermal effects on the location of ice stream marginsJournal of Geophysical Research, 1998
- Fracture mechanics approach to penetration of bottom crevasses on glaciersCold Regions Science and Technology, 1998
- Changes in the configuration of ice stream flow from the West Antarctic Ice SheetJournal of Geophysical Research, 1996
- High-resolution radar on Ice Stream B2, Antarctica: measurements of electromagnetic wave speed in firn and strain history from buried crevassesAnnals of Glaciology, 1994
- Irregular oscillations of the West Antarctic ice sheetNature, 1992
- AVHRR imagery reveals Antarctic ice dynamicsEos, 1990
- Ice-Shelf Response to Ice-stream Discharge Fluctuations: III. The Effects of Ice-stream Imbalance on the Ross Ice Shelf, AntarcticaJournal of Glaciology, 1989
- Water lubrication mechanism of glacier surgesCanadian Journal of Earth Sciences, 1969