Subglacial processes on an Antarctic ice stream bed. 2: Can modelled ice dynamics explain the morphology of mega-scale glacial lineations? (2016)
Attributed to:
The influence of evolving bed topography on marine ice stream stability.
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1017/jog.2016.19
Publication URI: http://dx.doi.org/10.1017/jog.2016.19
Type: Journal Article/Review
Parent Publication: Journal of Glaciology
Issue: 232