Sliding dominates slow-flowing margin regions, Greenland Ice Sheet

On the Greenland Ice Sheet (GrIS), ice flow due to deformation and sliding across the bed delivers ice to lower-elevation marginal regions where it can melt. We measured the two mechanisms of motion using a three-dimensional array of 212 tilt sensors installed within a network of boreholes drilled t...

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Detalles Bibliográficos
Autores principales: Maier, Nathan, Humphrey, Neil, Harper, Joel, Meierbachtol, Toby
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/PMC6620096/
https://www.ncbi.nlm.nih.gov/pubmed/31309154
http://dx.doi.org/10.1126/sciadv.aaw5406

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC6620096/
https://www.ncbi.nlm.nih.gov/pubmed/31309154
http://dx.doi.org/10.1126/sciadv.aaw5406

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