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• W2186430953 abstract "Narrow lateral shear margins are the most distinctive visual feature of theWest Antarctic ice streams. Large shear stresseswithinthese layerssupportthemajor- ity of the gravitational driving stress within a fast-flowing ice stream.The present contri- bution looks upstream, to the tributaries that feed ice-stream onsets, and considers the effects of both horizontal and vertical shear on their flow. Numerical and direct simula- tions of vertical and horizontal shear are used.Vertical shear, simulated using an aniso- tropic flow law, is of particular interest.We conclude that by isolating overlying ice from large-amplitude variations in bed elevation,``vertical shear margins''play an important role in sustaining relatively rapidtributary flow." @default.
• W2186430953 created "2016-06-24" @default.
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• W2186430953 date "2003-01-01" @default.
• W2186430953 modified "2023-09-27" @default.
• W2186430953 title "Therole of lateral andverticalshear intributary flow toward aWest Antarctic ice stream" @default.
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