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Complex Greenland outlet glacier flow captured

The Greenland Ice Sheet is losing mass at an accelerating rate due to increased surface melt and flow acceleration in outlet glaciers. Quantifying future dynamic contributions to sea level requires accurate portrayal of outlet glaciers in ice sheet simulations, but to date poor knowledge of subglaci...

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Detalles Bibliográficos
Autores principales:	Aschwanden, Andy, Fahnestock, Mark A., Truffer, Martin
Formato:	Online Artículo Texto
Lenguaje:	English
Publicado:	Nature Publishing Group 2016
Materias:	Article
Acceso en línea:	https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4740423/ https://www.ncbi.nlm.nih.gov/pubmed/26830316 http://dx.doi.org/10.1038/ncomms10524

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