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Greenland ice sheet motion insensitive to exceptional meltwater forcing

Changes to the dynamics of the Greenland ice sheet can be forced by various mechanisms including surface-melt–induced ice acceleration and oceanic forcing of marine-terminating glaciers. We use observations of ice motion to examine the surface melt–induced dynamic response of a land-terminating outl...

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Detalhes bibliográficos
Main Authors: Tedstone, Andrew J., Nienow, Peter W., Sole, Andrew J., Mair, Douglas W. F., Cowton, Thomas R., Bartholomew, Ian D., King, Matt A.
Formato: Artigo
Idioma:Inglês
Publicado em: National Academy of Sciences 2013
Assuntos:
Acesso em linha:https://ncbi.nlm.nih.gov/pmc/articles/PMC3856804/
https://ncbi.nlm.nih.gov/pubmed/24248343
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1073/pnas.1315843110
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