Low melt rates with seasonal variability at the base of Fimbul Ice Shelf, East Antarctica, revealed by in situ interferometric radar measurements
Author:
Affiliation:
1. Department of Geosciences; University of Oslo; Oslo Norway
2. Norwegian Polar Institute; Tromsø Norway
3. Norwegian Defence Research Establishment; Kjeller Norway
4. Akvaplan-niva; Tromsø Norway
Funder
Norwegian Research Council
NORKLIMA Norwegian Research Council
Publisher
American Geophysical Union (AGU)
Subject
General Earth and Planetary Sciences,Geophysics
Link
http://onlinelibrary.wiley.com/wol1/doi/10.1002/2014GL061782/fullpdf
Reference38 articles.
1. Ocean variability contributing to basal melt rate near the ice front of Ross Ice Shelf, Antarctica;Arzeno;J. Geophys. Res. Oceans,2014
2. Variability of basal melt beneath the Pine Island Glacier ice shelf, West Antarctica;Bindschadler;J. Glaciol.,2011
3. Reliability analysis for design of stake networks to measure glacier surface velocity;Chadwell;J. Glaciol.,1999
4. Precise measurement of changes in ice-shelf thickness by phase-sensitive radar to determine basal melt rates;Corr;Geophys. Res. Lett.,2002
5. Calving fluxes and basal melt rates of Antarctic ice shelves;Depoorter;Nature,2013
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