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Autor:
F. Vermassen, N. Andreasen, D. J. Wangner, N. Thibault, M.-S. Seidenkrantz, R. Jackson, S. Schmidt, K. H. Kjær, C. S. Andresen
Publikováno v:
Climate of the Past, Vol 15, Pp 1171-1186 (2019)
The mass loss from the Greenland Ice Sheet has increased over the past 2 decades. Marine-terminating glaciers contribute significantly to this mass loss due to increased melting and ice discharge. Periods of rapid retreat of these tidewater glaciers
Externí odkaz:
https://doaj.org/article/8442680b57144f018d9ff9e46e4295b7
