Identification and control of subglacial water networks under Dome A, Antarctica
Subglacial water in continental Antarctica forms by melting of basal ice due to geothermal or frictional heating. Subglacial networks transport the water from melting areas and can facilitate sliding by the ice sheet over its bed. Subglacial water flow is driven mainly by gradients in overburden pre...
| Main Authors: | , , , |
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| Format: | Text |
| Language: | unknown |
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Columbia University
2013
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| Subjects: | |
| Online Access: | https://dx.doi.org/10.7916/d8f769jn https://academiccommons.columbia.edu/doi/10.7916/D8F769JN |