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High geothermal heat flux in close proximity to the Northeast Greenland Ice Stream

The Greenland ice sheet (GIS) is losing mass at an increasing rate due to surface melt and flow acceleration in outlet glaciers. Currently, there is a large disagreement between observed and simulated ice flow, which may arise from inaccurate parameterization of basal motion, subglacial hydrology or...

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Detalles Bibliográficos
Autores principales:	Rysgaard, Søren, Bendtsen, Jørgen, Mortensen, John, Sejr, Mikael K.
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/PMC5777987/ https://www.ncbi.nlm.nih.gov/pubmed/29358631 http://dx.doi.org/10.1038/s41598-018-19244-x

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