Surface formation, preservation, and history of low-porosity crusts at the WAIS Divide site, West Antarctica
Observations at the West Antarctic Ice Sheet (WAIS) Divide site show that near-surface snow is strongly altered by weather-related processes such as strong winds and temperature fluctuations, producing features that are recognizable in the deep ice core. Prominent <q>glazed</q> surface c...
Published in: | The Cryosphere |
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Main Authors: | , , , , |
Format: | Text |
Language: | English |
Published: |
2018
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Subjects: | |
Online Access: | https://doi.org/10.5194/tc-12-325-2018 https://tc.copernicus.org/articles/12/325/2018/ |