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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Detalles Bibliográficos
Autores principales: Williams, C. Rosie, Hindmarsh, Richard C. A., Arthern, Robert J.
Formato: Online Artículo Texto
Lenguaje:English
Publicado: The Royal Society Publishing 2012
Materias:
Research Articles
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3509956/
https://www.ncbi.nlm.nih.gov/pubmed/23197934
http://dx.doi.org/10.1098/rspa.2012.0180

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC3509956/
https://www.ncbi.nlm.nih.gov/pubmed/23197934
http://dx.doi.org/10.1098/rspa.2012.0180

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