The internal melting of landfast sea ice in Prydz Bay, East Antarctica
Summertime internal melting of Antarctic sea ice is common due to the penetration of solar radiation below the snow and ice surface. We focus on the role of internal melting and heat conduction in generating gap layers within the ice. These often occur approximately 0.1 m below the ice surface. In a...
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| Auteurs principaux: | , , , , , |
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| Format: | Artigo |
| Langue: | Inglês |
| Publié: |
IOP Publishing
2022-01-01
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| Collection: | Environmental Research Letters |
| Sujets: | |
| Accès en ligne: | https://doi.org/10.1088/1748-9326/ac76d9 |
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