Tide induced velocity fluctuations in the grounding zone of Darwin Glacier, Antarctica, Revealed by GNSS and SAR satellite data.

Flow velocities and flow variations of Antarctic glaciers play an important role in Antarctica's mass balance and global sea level change. Oceanic tides are known to influence ice dynamics of outlet glaciers where they become afloat. The Darwin Glacier in the Transantarctic Mountains (TAM), Ant...

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Bibliographic Details
Main Author: Scheffler, Ekkehard
Format: Article in Journal/Newspaper
Language:English
Published: University of Canterbury 2017
Subjects:
Online Access:https://dx.doi.org/10.26021/6188
https://ir.canterbury.ac.nz/handle/10092/15629