Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability
Abstract
The marine portion of the West Antarctic Ice Sheet (WAIS) in the Amundsen Sea Embayment (ASE) accounts for one-fourth of the cryospheric contribution to global sea-level rise and is vulnerable to catastrophic collapse. The bedrock response to ice mass loss, glacial isostatic adjustment (GIA), was thought to occur on a time scale of 10,000 years. We used new GPS measurements, which show a rapid (41 millimeters per year) uplift of the ASE, to...
Paper Details
Title
Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability
Published Date
Jun 22, 2018
Journal
Volume
360
Issue
6395
Pages
1335 - 1339
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