Sheet, stream, and shelf flow as progressive ice-bed uncoupling: Byrd Glacier, Antarctica and Jakobshavn Isbrae, Greenland

• Published in: The Cryosphere
• Main Authors: T. Hughes, A. Sargent, J. Fastook, K. Purdon, J. Li, J.-B. Yan, S. Gogineni
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2016
• Subjects: Environmental sciences; GE1-350; Geology; QE1-996.5; Byrd; Byrd Glacier; Greenland; Antarc*; Antarctica; glacier; Ice Shelf; Jakobshavn; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-10-193-2016; https://doaj.org/article/a50a7a59a89a42f5a431ad96b0921199

The first-order control of ice thickness and height above sea level is linked to the decreasing strength of ice-bed coupling along flowlines from an interior ice divide to the calving front of an ice shelf. Uncoupling progresses as a frozen bed progressively thaws for sheet flow, as a thawed bed is...