Observations of surface mass balance on Pine Island Glacier, West Antarctica, and the effect of strain history in fast-flowing sections (2019)
Attributed to:
ISTAR-D - The contribution to sea-level rise of the Amundsen Sea sector of Antarctica
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.1017/jog.2019.36
Publication URI: http://dx.doi.org/10.1017/jog.2019.36
Type: Journal Article/Review
Parent Publication: Journal of Glaciology
Issue: 252