Complex multi-decadal ice dynamical change inland of marine-terminating glaciers on the Greenland Ice Sheet
Greenland's future contribution to sea-level rise is strongly dependent on the extent to which dynamic perturbations, originating at the margin, can drive increased ice flow within the ice-sheet interior. However, reported observations of ice dynamical change at distances >~50 km from the ma...
Main Authors: | , , |
---|---|
Format: | Article |
Language: | English |
Published: |
Cambridge University Press
2021-10-01
|
Series: | Journal of Glaciology |
Subjects: | |
Online Access: | https://www.cambridge.org/core/product/identifier/S0022143021000319/type/journal_article |