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...
Published in: | Annals of Glaciology |
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Main Authors: | , , |
Format: | Text |
Language: | unknown |
Published: |
Dartmouth Digital Commons
2016
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Subjects: | |
Online Access: | https://digitalcommons.dartmouth.edu/facoa/456 https://doi.org/10.1017/aog.2016.1 |