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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Detalles Bibliográficos
Autores principales: Spagnolo, Matteo, Phillips, Emrys, Piotrowski, Jan A., Rea, Brice R., Clark, Chris D., Stokes, Chris R., Carr, Simon J., Ely, Jeremy C., Ribolini, Adriano, Wysota, Wojciech, Szuman, Izabela
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group 2016
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4764869/
https://www.ncbi.nlm.nih.gov/pubmed/26898399
http://dx.doi.org/10.1038/ncomms10723

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC4764869/
https://www.ncbi.nlm.nih.gov/pubmed/26898399
http://dx.doi.org/10.1038/ncomms10723

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