Fun at Antarctic grounding lines: Ice-shelf channels and sediment transport

Meltwater beneath the polar ice sheets drains, in part, through subglacial conduits. Landforms created by such drainages are abundant in areas formerly covered by ice sheets during the last glacial maximum. However, observations of subglacial conduit dynamics under a contemporary ice sheet are lacki...

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Bibliographic Details
Main Authors: Drews, Reinhard, Mayer, Christoph, Eisen, Olaf, Helm, Veit, Ehlers, Todd, Pattyn, Frank, Berger, Sophie, Favier, Lionel, Hewitt, Ian H., Ng, Felix, Fürst, Johannes, Gillet-Chaulet, Fabien, Bergeot, Nicolas, Matsuoka, Kenichi
Format: Conference Object
Language:unknown
Published: 2017
Subjects:
Online Access:https://epic.awi.de/id/eprint/49626/
https://epic.awi.de/id/eprint/49626/1/EGU2017-12173.pdf
https://hdl.handle.net/10013/epic.7f3243c8-40b5-4436-81e4-48df805f2ba5
https://hdl.handle.net/