Radar-derived ice fabric anisotropy and implications on flow enhancement along the Thwaites Glacier Eastern Shear Margin (2023)
Attributed to:
Thwaites Interdisciplinary Margin Evolution (TIME)
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/egusphere-egu23-2178
Publication URI: http://dx.doi.org/10.5194/egusphere-egu23-2178
Type: Other