Persistence and variability of ice-stream grounding lines on retrograde bed slopes

• Published in: The Cryosphere
• Main Authors: Robel, Alexander A., Schoof, Christian, Tziperman, Eli
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2016
• Subjects: article; Verlagsveröffentlichung; West Antarctica; Antarc*; Antarctica; Ice Sheet; The Cryosphere
• Online Access: https://doi.org/10.5194/tc-10-1883-2016; https://noa.gwlb.de/receive/cop_mods_00011552; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00011509/tc-10-1883-2016.pdf; https://tc.copernicus.org/articles/10/1883/2016/tc-10-1883-2016.pdf

In many ice streams, basal resistance varies in space and time due to the dynamically evolving properties of subglacial till. These variations can cause internally generated oscillations in ice-stream flow. However, the potential for such variations in basal properties is not considered by conventional theories of grounding-line stability on retrograde bed slopes, which assume that bed properties are static in time. Using a flow-line model, we show how internally generated, transient variations in ice-stream state interact with retrograde bed slopes. In contrast to predictions from the theory of the marine ice-sheet instability, our simulated grounding line is able to persist and reverse direction of migration on a retrograde bed when undergoing oscillations in the grounding-line position. In turn, the presence of a retrograde bed may also suppress or reduce the amplitude of internal oscillations in ice-stream state. We explore the physical mechanisms responsible for these behaviors and discuss the implications for observed grounding-line migration in West Antarctica.