Titlebook: Dynamics of the West Antarctic Ice Sheet; Proceedings of a Wor C. J. Veen,J. Oerlemans Conference proceedings 1987 D. Reidel Publishing Com

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Amy Neustein,Judith A. Markowitze grounding line. The transition flow is found numerically by solving a non-linear elliptic differential equation with fixed boundary conditions. The transition zone is located around the grounding line and its width is of the order of the ice thickness. In the case of basal sliding the transition z

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https://doi.org/10.1007/978-1-4614-9123-1ge is 3 to 18 m./s at the grounding line. The inferred subglacial water pressure is greater than 90 % of the ice overburden pressure for the entire 300 km length of the ice stream, and greater than 96 % of the ice overburden pressure for 230 km upglacier from the grounding line. This suggests that t

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https://doi.org/10.1007/978-1-4615-0659-1 change. One of the most severe consequences alluded to is the possibility of a rapid rise in sea level resulting primarily from increased melting of the Antarctic Ice Sheet — particularly from West Antarctica where much of the ice is currently grounded well below sea level..The present generation o

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Dynamics of the West Antarctic Ice Sheet978-94-009-3745-1Series ISSN 0924-5006

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Women’s Entrepreneurship and Economics water reservoir). Nevertheless, small changes in ice volume can have large effects on sea level. For instance, a 1% change in ice volume results in a sea-level rise or drop of some 70 cm. So although the large ice caps are located in remote areas of the world, their evolution leaves a clear mark upon the regions in which we live.