Kinematic response of ice-rise divides to changes in ocean and atmosphere forcing

The majority of Antarctic ice shelves are bounded by grounded ice rises. These ice rises exhibit local flow fields that partially oppose the flow of the surrounding ice shelves. Formation of ice rises is accompanied by a characteristic upward-arching internal stratigraphy (“Raymond arches”), whose g...

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Bibliographic Details
Published in:The Cryosphere
Main Authors: Schannwell, Clemens, Drews, Reinhard, Ehlers, Todd A., Eisen, Olaf, Mayer, Christoph, Gillet-Chaulet, Fabien
Format: Text
Language:English
Published: 2019
Subjects:
Online Access:http://hdl.handle.net/10900/94103
https://doi.org/10.5194/tc-13-2673-2019
https://www.the-cryosphere.net/13/2673/2019/
https://doi.org/10.15496/publikation-35487