Large surface meltwater discharge from the Kangerlussuaq sector of the Greenland ice sheet during the record-warm year 2010 explained by detailed energy balance observations (2012)
Attributed to:
A holistic model of outlet calving, dynamic acceleration and drawdown for the Greenland Ice Sheet
funded by
NERC
Abstract
No abstract provided
Bibliographic Information
Digital Object Identifier: http://dx.doi.org/10.5194/tc-6-199-2012
Publication URI: http://dx.doi.org/10.5194/tc-6-199-2012
Type: Journal Article/Review
Parent Publication: The Cryosphere
Issue: 1