Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability

Valentina R. Barletta*, Michael Bevis, Benjamin E. Smith, Terry Wilson, Abel Brown, Andrea Bordoni, Michael Willis, Shfaqat Abbas Khan, Marc Rovira-Navarro, Ian Dalziel, Robert Smalley, Eric Kendrick, Stephanie Konfal, Dana J. Caccamise, Richard C. Aster, Andy Nyblade, Douglas A. Wiens

*Corresponding author for this work

Research output: Contribution to journalJournal articleResearchpeer-review

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 estimate the viscosity of the mantle underneath. We found a much lower viscosity (4 × 1018 pascal-second) than global average, and this shortens the GIA response time scale from tens to hundreds of years. Our finding requires an upward revision of ice mass loss from gravity data of 10% and increases the potential stability of the WAIS against catastrophic collapse.
Original languageEnglish
JournalScience
Volume360
Issue number6395
Pages (from-to)1335-1339
ISSN0036-8075
DOIs
Publication statusPublished - 2018

Fingerprint Dive into the research topics of 'Observed rapid bedrock uplift in Amundsen Sea Embayment promotes ice-sheet stability'. Together they form a unique fingerprint.

Cite this