Cryoconite Evolution and Formation on an Arctic Glacier Surface: A Case Study and Model, 2010

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 water abo...

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Bibliographic Details
Main Author: Terra Hittson
Format: Dataset
Language:unknown
Published: Arctic Data Center 2013
Subjects:
Online Access:https://doi.org/10.18739/A2K649S3H