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: C. Schannwell, R. Drews, T. A. Ehlers, O. Eisen, C. Mayer, F. Gillet-Chaulet
Format: Article in Journal/Newspaper
Language:English
Published: Copernicus Publications 2019
Subjects:
geo
Online Access:https://doi.org/10.5194/tc-13-2673-2019
https://www.the-cryosphere.net/13/2673/2019/tc-13-2673-2019.pdf
https://doaj.org/article/054f396b1ebb4aec86b7a51fea79572c