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Rate-and-state friction explains glacier surge propagation
The incomplete understanding of glacier dynamics is a major source of uncertainty in assessments of sea-level rise from land-based ice. Through increased ice discharge into the oceans, accelerating glacier flow has the potential to considerably enhance expected sea-level change, well ahead of scenar...
Guardat en:
| Publicat a: | Nat Commun |
|---|---|
| Autors principals: | , , , |
| Format: | Artigo |
| Idioma: | Inglês |
| Publicat: |
Nature Publishing Group UK
2019
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| Matèries: | |
| Accés en línia: | https://ncbi.nlm.nih.gov/pmc/articles/PMC6597537/ https://ncbi.nlm.nih.gov/pubmed/31249287 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41467-019-10506-4 |
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