Add to ORKGThis is the published version.Patterns of strain rate and slope on the ice streams are unusual. They cannot be accounted for in the usual way as due to standing waves in ice flow over a basal obstruction to flow (such as a sticky spot) . The features are studied using the force-budget technique. The conventional flow law is used, together with measurements of surface strain rate and shape of the glacier, to compute basal drag. The results for Ice Stream C are as expected, in that the drag varies from site to site but is directed inland, restraining the flow. The calculated drag at the base of Ice Stream B, on the other hand, is in places such that it acts to propel the glacier forward. This result is untenable. Either the convention...
Understanding the processes that affect streaming ice flow and the mass balance of glaciers and ice ...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...
This is the published version.Patterns of strain rate and slope on the ice streams are unusual. The...
Basal drag is a fundamental control on ice stream dynamics that remains poorly understood or constra...
This is the published version. Copyright 2014Force-balance calculations on Byrd Glacier, East Antarc...
This is the published version. Copyright 2014Force-balance calculations on Byrd Glacier, East Antarc...
Field data collected at the mouth of Ice Stream B show that the flow dynamics of this region are dis...
Force-balance calculations on Byrd Glacier, East Antarctica, reveal large spatial variations in the ...
This is the publisher's version, also available electronically from "http://www.ingentaconnect.com"....
This is the publisher's version, also available electronically from "http://www.ingentaconnect.com"....
Recent seismic studies of ice stream B, Antarctica and field analysis of mid-latitude glacial deposi...
AbstractDrag at the bed and along the lateral margins are the primary forces resisting flow in outle...
AbstractDrag at the bed and along the lateral margins are the primary forces resisting flow in outle...
ABSTRACT. Stresses at the surface and at depth are calculated for a stretch of Byrd Glacier, Antarct...
Understanding the processes that affect streaming ice flow and the mass balance of glaciers and ice ...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...
This is the published version.Patterns of strain rate and slope on the ice streams are unusual. The...
Basal drag is a fundamental control on ice stream dynamics that remains poorly understood or constra...
This is the published version. Copyright 2014Force-balance calculations on Byrd Glacier, East Antarc...
This is the published version. Copyright 2014Force-balance calculations on Byrd Glacier, East Antarc...
Field data collected at the mouth of Ice Stream B show that the flow dynamics of this region are dis...
Force-balance calculations on Byrd Glacier, East Antarctica, reveal large spatial variations in the ...
This is the publisher's version, also available electronically from "http://www.ingentaconnect.com"....
This is the publisher's version, also available electronically from "http://www.ingentaconnect.com"....
Recent seismic studies of ice stream B, Antarctica and field analysis of mid-latitude glacial deposi...
AbstractDrag at the bed and along the lateral margins are the primary forces resisting flow in outle...
AbstractDrag at the bed and along the lateral margins are the primary forces resisting flow in outle...
ABSTRACT. Stresses at the surface and at depth are calculated for a stretch of Byrd Glacier, Antarct...
Understanding the processes that affect streaming ice flow and the mass balance of glaciers and ice ...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...
This is the publisher's version, copyright by the International Glaciological Society.No abstract is...