Englacial and subglacial water flow at Skálafellsjökull, Iceland derived from ground penetrating radar, in situ Glacsweb probe and borehole water level measurements
We reconstruct englacial and subglacial drainage at Skálafellsjökull, Iceland, using ground penetrating radar (GPR) common offset surveys, borehole studies and Glacsweb probe data. We find that englacial water is not stored within the glacier (water content ~0-0.3%). Instead, the glacier is mostly...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
2015-12-04.
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| Subjects: | |
| Online Access: | Get fulltext Get fulltext |