Anisotropic Ice Flow Leading to the Onset of Ice Stream D, West Antarctica: Numerical Modelling Based on the Observations From Byrd Station Borehole

Annals of Glaciology- United Kingdom

doi 10.3189/172756403781815591

Full Text

Abstract

Available in

Date

Authors

Publisher

Cambridge University Press (CUP)

Related search

Force Balance Along an Inland Tributary and Onset to Ice Stream D, West Antarctica

Journal of Glaciology
Earth-Surface Processes
2002English

Development of Enhanced Ice Flow at the Southern Margin of Ice Stream D, Antarctica

Annals of Glaciology
Earth-Surface Processes
1994English

Ice-Core Insights Into the Flow and Shut-Down of Ice Stream C, West Antarctica

Annals of Glaciology
Earth-Surface Processes
2003English

Fast-Flow Signature in the Stagnated Kamb Ice Stream, West Antarctica

Geology
Geology
2004English

On the Formation of Blue Ice on Byrd Glacier, Antarctica

Journal of Glaciology
Earth-Surface Processes
2014English

Thickness Changes on Whillans Ice Stream and Ice Stream C, West Antarctica, Derived From Laser Altimeter Measurements

Journal of Glaciology
Earth-Surface Processes
2003English

Continued Deceleration of Whillans Ice Stream, West Antarctica

Geophysical Research Letters
EarthPlanetary SciencesGeophysics
2005English

Basal Friction of Ice Stream E, West Antarctica

Journal of Glaciology
Earth-Surface Processes
1995English

Mass Balance of Ice Stream B, West Antarctica

Annals of Glaciology
Earth-Surface Processes
1988English

Amanote Research

Note-taking for researchers

Follow Amanote

© 2026 Amaplex Software S.P.R.L. All rights reserved.

Privacy PolicyRefund Policy