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dc.contributor.authorJoughin, Ian
dc.date.accessioned2019-04-02T17:21:59Z
dc.date.available2019-04-02T17:21:59Z
dc.date.issued2019-04-01
dc.identifier.urihttp://hdl.handle.net/1773/43479
dc.description.abstractThe choice of the best basal friction law to use in ice-sheet models remains a source of uncertainty in projections of sea level. The parameters in commonly used friction laws can produce a broad range of behavior and are poorly constrained. Here we use a time series of elevation and speed data to examine the simulated transient response of Pine Island Glacier, Antarctica, to a loss of basal traction as its grounding line retreats. We evaluate a variety of friction laws, which produces a diversity of responses, to determine which best reproduces the observed speedup when forced with the observed thinning. Forms of the commonly used power-law friction provide much larger model-data disagreement than less commonly used regularized Coulomb friction in which cavitation effects yield an upper bound on basal friction. Thus, adoption of such friction laws could substantially improve the fidelity of large-scale simulations to determine future sea level.en_US
dc.language.isoen_USen_US
dc.rightsCC0 1.0 Universal*
dc.rights.urihttp://creativecommons.org/publicdomain/zero/1.0/*
dc.titleRegularized Coulomb Friction Laws for Ice Sheet Sliding: Application to Pine Island Glacier, Antarctica, [Data supporting Geophysical Res. Lett. Paper 2019GL082526R]en_US
dc.typeDataseten_US


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CC0 1.0 Universal
Except where otherwise noted, this item's license is described as CC0 1.0 Universal