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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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Kaydedildi:
Detaylı Bibliyografya
Yayımlandı:Sci Rep
Asıl Yazarlar: Rysgaard, Søren, Bendtsen, Jørgen, Mortensen, John, Sejr, Mikael K.
Materyal Türü: Artigo
Dil:Inglês
Baskı/Yayın Bilgisi: Nature Publishing Group UK 2018
Konular:
Online Erişim:https://ncbi.nlm.nih.gov/pmc/articles/PMC5777987/
https://ncbi.nlm.nih.gov/pubmed/29358631
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1038/s41598-018-19244-x
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