Cyclic behaviour on millennial time scale due to creep instabilities in western Dronning Maud Land, Antarctica

At the base of a thick ice sheet the temperature locally reaches the pressure melting point and melting generates a thin subglacial water layer. The basal water lubricates the base and thus enhances the sliding of the ice sheet. As a consequence of sliding, the heat source of internal strain heating...

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Bibliographic Details
Main Authors: Kleiner, Thomas, Humbert, Angelika
Format: Conference Object
Language:unknown
Published: Geophysical Research Abstracts 2013
Subjects:
Online Access:https://epic.awi.de/id/eprint/32911/
https://epic.awi.de/id/eprint/32911/1/EGU2013-9732.pdf
https://hdl.handle.net/10013/epic.41449
https://hdl.handle.net/10013/epic.41449.d001