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Frequency response of ice streams
Changes at the grounding line of ice streams have consequences for inland ice dynamics and hence sea level. Despite substantial evidence documenting upstream propagation of frontal change, the mechanisms by which these changes are transmitted inland are not well understood. In this vein, the frequen...
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| Main Authors: | , , |
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| Formato: | Artigo |
| Idioma: | Inglês |
| Publicado em: |
The Royal Society Publishing
2012
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| Assuntos: | |
| Acesso em linha: | https://ncbi.nlm.nih.gov/pmc/articles/PMC3509956/ https://ncbi.nlm.nih.gov/pubmed/23197934 https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1098/rspa.2012.0180 |
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