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pro vyhledávání: '"R. M. Antwerpen"'
Publikováno v:
The Cryosphere, Vol 16, Pp 4185-4199 (2022)
Surface mass loss from the Greenland ice sheet (GrIS) has accelerated over the past decades, mainly due to enhanced surface melting and liquid water runoff in response to atmospheric warming. A large portion of runoff from the GrIS originates from ex
Externí odkaz:
https://doaj.org/article/62ebe9d61aab439c85594bca8694ebd1