Use of a new finite element continuity model to study the transient behavior of ice stream C and causes of its present low velocity
- 10 August 1987
- journal article
- Published by American Geophysical Union (AGU) in Journal of Geophysical Research
- Vol. 92 (B9) , 8941-8949
- https://doi.org/10.1029/jb092ib09p08941
Abstract
No abstract availableKeywords
This publication has 4 references indexed in Scilit:
- Seismic measurements reveal a saturated porous layer beneath an active Antarctic ice streamNature, 1986
- RISS, RISP and RIGGS: Post-IGY glaciological investigations of the Ross Ice Shelfin the U.S. programmeJournal of the Royal Society of New Zealand, 1981
- The Theory of Glacier SlidingJournal of Glaciology, 1964
- The creep of polycrystalline iceProceedings of the Royal Society of London. Series A. Mathematical and Physical Sciences, 1955