Cargando…
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,...
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: | |
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 |
Ejemplares similares
-
Ice-stream demise dynamically conditioned by trough shape and bed strength
por: Bradwell, Tom, et al.
Publicado: (2019) -
High spatial and temporal variability in Antarctic ice discharge linked to ice shelf buttressing and bed geometry
por: Miles, Bertie W. J., et al.
Publicado: (2022) -
A Generalized Interpolation Material Point Method for Shallow Ice Shelves. 1: Shallow Shelf Approximation and Ice Thickness Evolution
por: Huth, Alex, et al.
Publicado: (2021) -
Atmospheric circulation over Europe during the Younger Dryas
por: Rea, Brice R., et al.
Publicado: (2020) -
Frequency response of ice streams
por: Williams, C. Rosie, et al.
Publicado: (2012)