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...
Main Authors: | , |
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Format: | Conference Object |
Language: | unknown |
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Geophysical Research Abstracts
2013
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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 |