Melting and freezing beneath the Ross ice streams, Antarctica
- 1 January 2004
- journal article
- Published by International Glaciological Society in Journal of Glaciology
- Vol. 50 (168) , 96-108
- https://doi.org/10.3189/172756504781830295
Abstract
No abstract availableKeywords
This publication has 45 references indexed in Scilit:
- Response of subglacial sediments to basal freeze‐on 2. Application in numerical modeling of the recent stoppage of Ice Stream C, West AntarcticaJournal of Geophysical Research, 2003
- Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice ShelfGeophysical Research Letters, 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
- Sub‐catchment melt and long‐term stability of ice stream D, West AntarcticaGeophysical Research Letters, 2002
- Force balance along an inland tributary and onset to Ice Stream D, West AntarcticaJournal of Glaciology, 2002
- Evidence for a recently abandoned shear margin adjacent to ice stream B2, Antarctica, from ice‐penetrating radar measurementsJournal of Geophysical Research, 2000
- Basal mechanics of Ice Stream B, west Antarctica: 2. Undrained plastic bed modelJournal of Geophysical Research, 2000
- A new numerical model of coupled inland ice sheet, ice stream, and ice shelf flow and its application to the West Antarctic Ice SheetJournal of Geophysical Research, 1999
- Binge/purge oscillations of the Laurentide Ice Sheet as a cause of the North Atlantic's Heinrich eventsPaleoceanography and Paleoclimatology, 1993
- Antarctic Ice Sheet: Preliminary Results of First Core Hole to BedrockScience, 1968