Decadal Ocean Forcing and Antarctic Ice Sheet Response: Lessons from the Amundsen Sea

Mass loss from the Antarctic Ice Sheet is driven by changes at the marine margins. In the Amundsen Sea, thinning of the ice shelves has allowed the outlet glaciers to accelerate and thin, resulting in inland migration of their grounding lines. The ultimate driver is often assumed to be ocean warming...

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Bibliographic Details
Main Authors: Adrian Jenkins, Pierre Dutrieux, Stan Jacobs, Eric J. Steig, G. Hilmar Gudmundsson, James Smith, Karen J. Heywood
Format: Article
Language:English
Published: The Oceanography Society 2016-12-01
Series:Oceanography
Subjects:
Online Access:https://tos.org/oceanography/assets/docs/29-4_jenkins.pdf