Cascading lake drainage on the Greenland Ice Sheet triggered by tensile shock and fracture

Supraglacial lakes on the Greenland Ice Sheet are expanding inland, but the impact on ice flow is equivocal because interior surface conditions may preclude the transfer of surface water to the bed. Here we use a well-constrained 3D model to demonstrate that supraglacial lakes in Greenland drain whe...

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Detalles Bibliográficos
Autores principales: Christoffersen, Poul, Bougamont, Marion, Hubbard, Alun, Doyle, Samuel H., Grigsby, Shane, Pettersson, Rickard
Formato: Online Artículo Texto
Lenguaje:English
Publicado: Nature Publishing Group UK 2018
Materias:
Article
Acceso en línea:https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5852115/
https://www.ncbi.nlm.nih.gov/pubmed/29540693
http://dx.doi.org/10.1038/s41467-018-03420-8

Internet

https://www.ncbi.nlm.nih.gov/pmc/articles/PMC5852115/
https://www.ncbi.nlm.nih.gov/pubmed/29540693
http://dx.doi.org/10.1038/s41467-018-03420-8

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