Hydraulic Conductivity of a Firn Aquifer in Southeast Greenland

Some regions of the Greenland ice sheet, where snow accumulation and melt rates are high, currently retain substantial volumes of liquid water within the firn pore space throughout the year. These firn aquifers, found between ~10 and 30 m below the snow surface, may significantly affect sea level ri...

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Autors principals:	Olivia L. Miller, D. Kip Solomon, Clément Miège, Lora S. Koenig, Richard R. Forster, Lynn N. Montgomery, Nicholas Schmerr, Stefan R. M. Ligtenberg, Anatoly Legchenko, Ludovic Brucker
Format:	Artigo
Idioma:	Inglês
Publicat:	Frontiers Media S.A. 2017-05-01
Col·lecció:	Frontiers in Earth Science
Matèries:	hydraulic conductivity mass balance aquifer test slug test meltwater flow
Accés en línia:	http://journal.frontiersin.org/article/10.3389/feart.2017.00038/full
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