Subglacial hydrology at Rink Isbræ, West Greenland inferred from sediment plume appearance

Marine-terminating outlet glaciers discharge most of the Greenland ice sheet’s mass through frontal ablation and meltwater runoff. While calving can be estimated by in situ and remote sensing observations, submarine melting and subglacial meltwater transport are more challenging to quantify. Here we...

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Bibliographic Details
Published in:Annals of Glaciology
Main Authors: Schild, Kristin M, Hawley, Robert L, Morriss, Blaine F
Format: Text
Language:unknown
Published: Dartmouth Digital Commons 2016
Subjects:
Online Access:https://digitalcommons.dartmouth.edu/facoa/456
https://doi.org/10.1017/aog.2016.1