Active water exchange and life near the grounding line of an Antarctic outlet glacier

The grounding line (GL) of the Antarctic ice sheet forms the boundary between grounded and floating ice along the coast. Near this line, warm oceanic water contacts the ice shelf, producing the ice sheet's highest basal-melt rate. Despite the importance of this region, water properties and circ...

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Bibliographic Details
Published in:Earth and Planetary Science Letters
Main Authors: Sugiyama, Shin, Sawagaki, Takanobu, Fukuda, Takehiro, Aoki, Shigeru
Format: Article in Journal/Newspaper
Language:English
Published: Elsevier
Subjects:
450
Online Access:http://hdl.handle.net/2115/57003
https://doi.org/10.1016/j.epsl.2014.05.001