Seismic evidence for complex sedimentary control of Greenland Ice Sheet flow

The land-terminating margin of the Greenland Ice Sheet has slowed down in recent decades, although the causes and implications for future ice flow are unclear. Explained originally by a self-regulating mechanism where basal slip reduces as drainage evolves from low to high efficiency, recent numeric...

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Pubblicato in:Sci Adv
Autori principali: Kulessa, Bernd, Hubbard, Alun L., Booth, Adam D., Bougamont, Marion, Dow, Christine F., Doyle, Samuel H., Christoffersen, Poul, Lindbäck, Katrin, Pettersson, Rickard, Fitzpatrick, Andrew A. W., Jones, Glenn A.
Natura: Artigo
Lingua:Inglês
Pubblicazione: American Association for the Advancement of Science 2017
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Research Articles
Accesso online:https://ncbi.nlm.nih.gov/pmc/articles/PMC5559208/
https://ncbi.nlm.nih.gov/pubmed/28835915
https://ncbi.nlm.nih.govhttp://dx.doi.org/10.1126/sciadv.1603071
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