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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Detalles Bibliográficos

Principais autores:	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
Formato:	Artigo
Idioma:	Inglês
Publicado:	Frontiers Media S.A. 2017-05-01
Series:	Frontiers in Earth Science
Assuntos:	hydraulic conductivity mass balance aquifer test slug test meltwater flow
Acceso en liña:	http://journal.frontiersin.org/article/10.3389/feart.2017.00038/full
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