Evidence for variable grounding-zone and shear-margin basal conditions across Thwaites Glacier, West Antarctica
Author:
Affiliation:
1. California Institute of Technology, Jet Propulsion Laboratory, Pasadena, California, USA..
2. University of Texas at Austin, Institute for Geophysics, Austin, Texas, USA..
Abstract
Publisher
Society of Exploration Geophysicists
Subject
Geochemistry and Petrology,Geophysics
Link
https://library.seg.org/doi/pdf/10.1190/geo2015-0122.1
Reference40 articles.
1. Reassessment of the Potential Sea-Level Rise from a Collapse of the West Antarctic Ice Sheet
2. Bed reflectivity beneath inactive ice streams in West Antarctica
3. Ice sheet grounding zone stabilization due to till compaction
4. Strong Sensitivity of Pine Island Ice-Shelf Melting to Climatic Variability
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