Multiple Steady States in Ice-Water-Till Systems
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An ice sheet with fixed boundary conditions may have two steady configurations, as shown by a new one-dimensional model including the physics and continuity of ice, water, and deforming subglacial till. In one steady state, a steep surface slope causes rapid internal ice shearing but forces basal water through subglacial aquifers, suppressing basal velocity; in the other steady state, a gentle surface slope causes only slow ice shearing but allows water to lubricate the ice-bed interface and cause rapid basal velocities. Small climatic forcing may cause large ice-sheet response during a switch between steady states.
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2012 ◽
Vol 17
(6)
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pp. 1227-1251
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2018 ◽
Vol 24
(2)
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pp. 765-792
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Philosophical Transactions of the Royal Society of London Series A Physical and Engineering Sciences
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1992 ◽
Vol 339
(1654)
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pp. 387-394
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2016 ◽
Vol 26
(04)
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pp. 1650066
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1999 ◽
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2000 ◽
Vol 26
(7)
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pp. 1095-1115
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1995 ◽
Vol 100
(D8)
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pp. 16265
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