Ice stream D flow speed is strongly modulated by the tide beneath the Ross Ice Shelf
Top Cited Papers
- 2 April 2003
- journal article
- Published by American Geophysical Union (AGU) in Geophysical Research Letters
- Vol. 30 (7)
- https://doi.org/10.1029/2002gl016329
Abstract
No abstract availableThis publication has 20 references indexed in Scilit:
- Tidal observations on floating ice using a single GPS receiverGeophysical Research Letters, 2003
- Earth tide forcing of glacier drainageGeophysical Research Letters, 2003
- Tidally driven stick–slip motion in the mouth of Whillans Ice Stream, AntarcticaAnnals of Glaciology, 2003
- Tide‐induced lateral movement of Brunt Ice Shelf, AntarcticaGeophysical Research Letters, 2002
- A new tide model for the Antarctic ice shelves and seasAnnals of Glaciology, 2002
- Continuity comes first: recent progress in understanding subglacial deformationGeological Society, London, Special Publications, 2000
- Tributaries of West Antarctic Ice Streams Revealed by RADARSAT InterferometryScience, 1999
- Tidal forcing of basal seismicity of ice stream C, West Antarctica, observed far inlandJournal of Geophysical Research, 1997
- Precise point positioning for the efficient and robust analysis of GPS data from large networksJournal of Geophysical Research, 1997
- Satellite Radar Interferometry for Monitoring Ice Sheet Motion: Application to an Antarctic Ice StreamScience, 1993