Modelled fracture and calving on the Totten Ice Shelf

• Published in: The Cryosphere
• Main Authors: Cook, Sue, Åström, Jan, Zwinger, Thomas, Galton-Fenzi, Benjamin Keith, Greenbaum, Jamin Stevens, Coleman, Richard
• Format: Article in Journal/Newspaper
• Language: English
• Published: Copernicus Publications 2018
• Subjects: article; Verlagsveröffentlichung; Ice Sheet; Ice Shelf; The Cryosphere; Totten Ice Shelf
• Online Access: https://doi.org/10.5194/tc-12-2401-2018; https://noa.gwlb.de/receive/cop_mods_00005220; https://noa.gwlb.de/servlets/MCRFileNodeServlet/cop_derivate_00005177/tc-12-2401-2018.pdf; https://tc.copernicus.org/articles/12/2401/2018/tc-12-2401-2018.pdf

The Totten Ice Shelf (IS) has a large drainage basin, much of which is grounded below sea level, leaving the glacier vulnerable to retreat through the marine ice sheet instability mechanism. The ice shelf has also been shown to be sensitive to changes in calving rate, as a very small retreat of the calving front from its current position is predicted to cause a change in flow at the grounding line. Therefore understanding the processes behind calving on the Totten IS is key to predicting its future sea level rise contribution. Here we use the Helsinki Discrete Element Model (HiDEM) to show that not all of the fractures visible at the front of the Totten IS are produced locally, but that the across-flow basal crevasses, which are part of the distinctive cross-cutting fracture pattern, are advected into the calving front area from upstream. A separate simulation of the grounding line shows that re-grounding points may be key areas of basal crevasse production, and can produce basal crevasses in both an along- and across-flow orientation. The along-flow basal crevasses at the grounding line may be a possible precursor to basal channels, while we suggest the across-flow grounding-line fractures are the source of the across-flow features observed at the calving front. We use two additional models to simulate the evolution of basal fractures as they advect downstream, demonstrating that both strain and ocean melt have the potential to deform narrow fractures into the broad basal features observed near the calving front. The wide range of factors which influence fracture patterns and calving on this glacier will be a challenge for predicting its future mass loss.