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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Format: | Article in Journal/Newspaper |
Language: | English |
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University of Canterbury
2017
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Online Access: | https://dx.doi.org/10.26021/6188 https://ir.canterbury.ac.nz/handle/10092/15629 |