Dynamics of the snow grain size in a windy coastal area of Antarctica from continuous in situ spectral-albedo measurements
<p>The grain size of the superficial snow layer is a key determinant of the surface albedo in Antarctica. Its evolution is the result of multiple interacting processes, such as dry and wet metamorphism, melt, snow drift, and precipitation. Among them, snow drift has the least known and least p...
| Main Authors: | , , , |
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| Format: | Article |
| Language: | English |
| Published: |
Copernicus Publications
2023-06-01
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| Series: | The Cryosphere |
| Online Access: | https://tc.copernicus.org/articles/17/2323/2023/tc-17-2323-2023.pdf |