In-situ quantification of ice rheology and direct measurement of the Raymond Effect at Summit, Greenland using a phase-sensitive radar IN-SITU QUANTIFICATION OF ICE RHEOLOGY (2011)
Attributed to:
Measuring and modelling the Raymond Effect for to infer low strain-rate ice rheology
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1029/2011gl049843
Publication URI: http://dx.doi.org/10.1029/2011gl049843
Type: Journal Article/Review
Parent Publication: Geophysical Research Letters
Issue: 24