Hittson 2010 Cryoconite Evolution and Formation on an Arctic Glacier Surface: A Case Study and Model
Abstract: Cryoconite holes are vertical cylindrical holes that form on glacier surfaces due to the lower albedo of sediments. Cryoconite holes exist on Linnebreen, Svalbard over the entirety of the glacier. They preferentially melt below the surrounding glacier surface and eventually create standing...
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Format: | Dataset |
Language: | unknown |
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Arctic Data Center
2013
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Online Access: | https://doi.org/10.18739/A2H60W |