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Ice stream motion facilitated by a shallow-deforming and accreting bed
Ice streams drain large portions of ice sheets and play a fundamental role in governing their response to atmospheric and oceanic forcing, with implications for sea-level change. The mechanisms that generate ice stream flow remain elusive. Basal sliding and/or bed deformation have been hypothesized,...
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| Publicado no: | Nat Commun |
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| Main Authors: | , , , , , , , , , , |
| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
Nature Publishing Group
2016
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC4764869/ https://ncbi.nlm.nih.gov/pubmed/26898399 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/ncomms10723 |
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