Accelerated heterogeneous retreat of Thwaites glacier, West Antarctica, fueled by high subaqueous melting at the grounding line.
The glaciers flowing into West Antarctica’s Amundsen Sea Embayment (ASE) have been characterized by significant changes during the last decades including acceleration, grounding line retreat and a positive mass imbalance. Here we measure Thwaites glacier draining the Amundsen Sea sector of West Anta...
Main Authors: | , , , , , , |
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Format: | Conference Object |
Language: | unknown |
Published: |
2019
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Subjects: | |
Online Access: | https://elib.dlr.de/127177/ |