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...

Full description

Bibliographic Details
Main Authors: Joel Harper, Toby Meierbachtol
Format: Dataset
Language:unknown
Published: Arctic Data Center 2019
Subjects:
Online Access:https://search.dataone.org/view/urn:uuid:4e300537-0ad7-4a78-92e6-0aa909e2fab6