Ice microstructure (electron backscatter diffraction) from Jarvis Glacier, Alaska, 2017-2020
Ice sheets and alpine glaciers discharge primarily though streaming flow, so the dynamics of that flow is central to the overall mass balance of the cryosphere. In glaciers and ice streams, the resistance to flow at the bed is important, but equally important is the internal viscous strength of the...
| Main Authors: | , |
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| Format: | Dataset |
| Language: | English |
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NSF Arctic Data Center
2020
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| Online Access: | https://dx.doi.org/10.18739/a2gb1xh9k https://arcticdata.io/catalog/view/doi:10.18739/A2GB1XH9K |