Inversion for the density-depth profile of polar firn using a stepped-frequency radar (2013)
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/10.1002/jgrf.20089
Publication URI: http://dx.doi.org/10.1002/jgrf.20089
Type: Journal Article/Review
Parent Publication: Journal of Geophysical Research: Earth Surface
Issue: 3