Transition from a subaerial to a subnival permafrost temperature regime following increased snow cover (Livingston Island, maritime antarctic)

1. Ramos, M.
2. Vieira, G.
3. de Pablo, M.A.
4. Molina, A.
5. Jimenez, J.J.

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DOI: 10.3390/ATMOS11121332 GOOGLE SCHOLAR lock_openOpen access editor

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