The future sea-level contribution of the Greenland ice sheet: a multi-model ensemble study of ISMIP6

<p>The Greenland ice sheet is one of the largest contributors to global mean sea-level rise today and is expected to continue to lose mass as the Arctic continues to warm. The two predominant mass loss mechanisms are increased surface meltwater run-off and mass loss associated with the retreat of ma...

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Autors principals:	H. Goelzer, S. Nowicki, A. Payne, E. Larour, H. Seroussi, W. H. Lipscomb, J. Gregory, A. Abe-Ouchi, A. Shepherd, E. Simon, C. Agosta, P. Alexander, A. Aschwanden, A. Barthel, R. Calov, C. Chambers, Y. Choi, J. Cuzzone, C. Dumas, T. Edwards, D. Felikson, X. Fettweis, N. R. Golledge, R. Greve, A. Humbert, P. Huybrechts, S. Le clec'h, V. Lee, G. Leguy, C. Little, D. P. Lowry, M. Morlighem, I. Nias, A. Quiquet, M. Rückamp, N.-J. Schlegel, D. A. Slater, R. S. Smith, F. Straneo, L. Tarasov, R. van de Wal, M. van den Broeke
Format:	Artigo
Idioma:	Inglês
Publicat:	Copernicus Publications 2020-09-01
Col·lecció:	The Cryosphere
Matèries:	open climate campaign
Accés en línia:	https://tc.copernicus.org/articles/14/3071/2020/tc-14-3071-2020.pdf
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