Ice-stream demise dynamically conditioned by trough shape and bed strength

Ice sheet mass loss is currently dominated by fast-flowing glaciers (ice streams) terminating in the ocean as ice shelves and resting on beds below sea level. The factors controlling ice-stream flow and retreat over longer time scales (>100 years), especially the role of three-dimensional bed sha...

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Detalles Bibliográficos
Autores principales: Bradwell, Tom, Small, David, Fabel, Derek, Smedley, Rachel K., Clark, Chris D., Saher, Margot H., Callard, S. Louise, Chiverrell, Richard C., Dove, Dayton, Moreton, Steven G., Roberts, David H., Duller, Geoff A. T., Ó Cofaigh, Colm
Formato: Online Artículo Texto
Lenguaje:English
Publicado: American Association for the Advancement of Science 2019
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6498188/
https://www.ncbi.nlm.nih.gov/pubmed/31058217
http://dx.doi.org/10.1126/sciadv.aau1380

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6498188/
https://www.ncbi.nlm.nih.gov/pubmed/31058217
http://dx.doi.org/10.1126/sciadv.aau1380

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