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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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| Udgivet i: | Sci Adv |
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| Main Authors: | , , , , , , , , , , , , |
| Format: | Artigo |
| Sprog: | Inglês |
| Udgivet: |
American Association for the Advancement of Science
2019
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| Fag: | |
| Online adgang: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6498188/ https://ncbi.nlm.nih.gov/pubmed/31058217 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.aau1380 |
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