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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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Main Authors: | , , , , , , |
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Formato: | Artigo |
Idioma: | Inglês |
Publicado em: |
National Academy of Sciences
2013
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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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