Collaborative Research: In Situ Borehole Measurements To Partition The Velocity Of The Greenland Ice Sheet Into Ice Deformation And Basal Sliding Components, 2014-2017
Sliding of an ice mass along its basal boundary is a fundamental component of motion where bed conditions are wet. Estimates of basal sliding generally result from an inverse analysis of observed surface motion using a model assuming Glen's generalized constitutive law for isotropic ice. Eviden...
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Arctic Data Center
2019
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Online Access: | https://search.dataone.org/view/urn:uuid:4e300537-0ad7-4a78-92e6-0aa909e2fab6 |