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 zone can be widened considerably.

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https://doi.org/10.1007/978-94-009-3745-1Ice shelf; Scale; atmosphere; climate; subglacial; temperature; water; hydrogeology

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Evaluating Complex Development ProgramsWe report here on some of the results of our first two seasons work along the Siple Coast. These results are all preliminary in nature and could be modified substantially with further analysis. Furthermore, we have selected from a much larger body of data only a few points that we believe will be of interest to this workshop.

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A Few Preliminary Results from the Glaciogeophysical Survey of the Interior Ross Embayment (GSIRE),We report here on some of the results of our first two seasons work along the Siple Coast. These results are all preliminary in nature and could be modified substantially with further analysis. Furthermore, we have selected from a much larger body of data only a few points that we believe will be of interest to this workshop.

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The West Antarctic Ice Sheet: The Need to Understand Its Dynamics, 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 up

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Quantitative Estimates of the Mass Flux and Ice Movement Along the Ice Edges in the Eastern and Sou apparent ice movements for the period under consideration, i.e. apparent advance rates and azimuths of ice-edge alteration during particular time intervals. The near-ice-edge movements thus determined are in good agreement with the ice movement as derived from interpretation of Landsat images and W