Ice Stream B Margin Revisited
Ice stream margins are some of the most interesting natural ice dynamics laboratories. Large temperature differences between the base and the surface of the ice stream cause large variations in the ice flow parameter. Ice traversing the margins is exposed to large strains. This is expected to lead t...
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ftciteseerx:oai:CiteSeerX.psu:10.1.1.524.5189 2023-05-15T16:41:09+02:00 Ice Stream B Margin Revisited Martin Truffer Keith Echelmeyer The Pennsylvania State University CiteSeerX Archives application/pdf http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.5189 http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf en eng http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.5189 http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf Metadata may be used without restrictions as long as the oai identifier remains attached to it. http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf text ftciteseerx 2016-01-08T10:17:47Z Ice stream margins are some of the most interesting natural ice dynamics laboratories. Large temperature differences between the base and the surface of the ice stream cause large variations in the ice flow parameter. Ice traversing the margins is exposed to large strains. This is expected to lead to an alignment of c-axis and a consequent softening of the ice in lateral shear. Echelmeyer and others (1994) used a finite element model to show that the very steep velocity gradients across the ice stream margin could only be reproduced if the ice in the margins is up to ten times softer than the adjacent ice sheet ice. We repeated this modeling effort using a more accurate ice stream geometry, and adjusting the ice flow parameters for ice temperatures that have been measured in the mean time. Reproducing the measured surface velocity profiles still requires enhancement factors of about ten. Since the temperature effects have been accounted for we conclude that these enhancement factors are due to fabric changes in the marginal ice. Method A commercial Finite Element package (FEMLAB(R)) was adapted to solve the non-linear ice flow equations. The method solves for all three velocity components and their gradients in a plane. It does not account for out-of-plane velocity gradients, however. It is possible to specify velocities or stresses at the model boundaries. Text Ice Sheet Ice Stream B Unknown |
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English |
description |
Ice stream margins are some of the most interesting natural ice dynamics laboratories. Large temperature differences between the base and the surface of the ice stream cause large variations in the ice flow parameter. Ice traversing the margins is exposed to large strains. This is expected to lead to an alignment of c-axis and a consequent softening of the ice in lateral shear. Echelmeyer and others (1994) used a finite element model to show that the very steep velocity gradients across the ice stream margin could only be reproduced if the ice in the margins is up to ten times softer than the adjacent ice sheet ice. We repeated this modeling effort using a more accurate ice stream geometry, and adjusting the ice flow parameters for ice temperatures that have been measured in the mean time. Reproducing the measured surface velocity profiles still requires enhancement factors of about ten. Since the temperature effects have been accounted for we conclude that these enhancement factors are due to fabric changes in the marginal ice. Method A commercial Finite Element package (FEMLAB(R)) was adapted to solve the non-linear ice flow equations. The method solves for all three velocity components and their gradients in a plane. It does not account for out-of-plane velocity gradients, however. It is possible to specify velocities or stresses at the model boundaries. |
author2 |
The Pennsylvania State University CiteSeerX Archives |
format |
Text |
author |
Martin Truffer Keith Echelmeyer |
spellingShingle |
Martin Truffer Keith Echelmeyer Ice Stream B Margin Revisited |
author_facet |
Martin Truffer Keith Echelmeyer |
author_sort |
Martin Truffer |
title |
Ice Stream B Margin Revisited |
title_short |
Ice Stream B Margin Revisited |
title_full |
Ice Stream B Margin Revisited |
title_fullStr |
Ice Stream B Margin Revisited |
title_full_unstemmed |
Ice Stream B Margin Revisited |
title_sort |
ice stream b margin revisited |
url |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.5189 http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf |
genre |
Ice Sheet Ice Stream B |
genre_facet |
Ice Sheet Ice Stream B |
op_source |
http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf |
op_relation |
http://citeseerx.ist.psu.edu/viewdoc/summary?doi=10.1.1.524.5189 http://www2.gi.alaska.edu/~truffer/WAIS_poster.pdf |
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Metadata may be used without restrictions as long as the oai identifier remains attached to it. |
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