Ice-stream flow switching during deglaciation of the southwestern Barents Sea.
Ice streams dominate the discharge of continental ice sheets. Recent observations and reconstructions have revealed that large-scale reorganizations in their flow trajectory (flow switching) can occur over relatively short time scales. However, the underlying causes of such behavior, and the extent...
Published in: | Geological Society of America Bulletin |
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Main Authors: | , , |
Format: | Article in Journal/Newspaper |
Language: | unknown |
Published: |
Geological Society of America
2012
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Subjects: | |
Online Access: | http://dro.dur.ac.uk/11094/ https://doi.org/10.1130/B30416.1 |