Ice Stream C slowdown is not stabilizing West Antarctic Ice Sheet

Changes in the flow of ice stream C likely indicate a continuing slow drawdown of the Siple Coast of West Antarctica rather than a stabilizing feedback. The downglacier part of ice stream C, West Antarctica largely stagnated over the last few centuries, while upglacier regions continue to flow vigor...

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Bibliographic Details
Main Authors: S Anandakrishnan, Rb Alley, Rw Jacobel, H Conway
Other Authors: The Pennsylvania State University CiteSeerX Archives
Format: Text
Language:English
Published: 1999
Subjects:
Online Access:http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.366.9711
http://www.stolaf.edu/other/cegsic/publications/Anandakrishnan et al.pdf