Black Rapids glacier GPS data, Eastern Alaska Range, 2012-2014
A glacier surge is characterized by a sudden increase in speed by one to two orders of magnitude and often leads to a significant movement of the terminus of the glacier. While the role of subglacial hydraulics during the surge has been well documented, the issue of surge initiation has remained uns...
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| Format: | Dataset |
| Language: | English |
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NSF Arctic Data Center
2017
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| Online Access: | https://dx.doi.org/10.18739/a2w950p3n https://arcticdata.io/catalog/view/doi:10.18739/A2W950P3N |
| Summary: | A glacier surge is characterized by a sudden increase in speed by one to two orders of magnitude and often leads to a significant movement of the terminus of the glacier. While the role of subglacial hydraulics during the surge has been well documented, the issue of surge initiation has remained unsolved. Also, the related question of why some glaciers surge and others do not remains open. This data set supported work to investigate whether the special geometry of many Alaska Range glaciers allows particularly large shear stresses to develop that eventually allow a surge to occur. The work focused on the Black Rapids Glacier on the Denali Fault in the eastern Alaska Range. This data set contains GPS measurements that were used to derive ice velocities. The velocities are used to document glacier speed-up events that occur annually as marginal lakes drain to the glacier bed and lubricate it. Such events act like mini-surges. Particular emphasis is placed on the reaction of tributary glaciers to a speed-up of the main branch. |
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