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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| Asıl Yazarlar: | , , , , , , , , , |
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| Materyal Türü: | Artigo |
| Dil: | Inglês |
| Baskı/Yayın Bilgisi: |
Frontiers Media S.A.
2017-05-01
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| Seri Bilgileri: | Frontiers in Earth Science |
| Konular: | |
| Online Erişim: | http://journal.frontiersin.org/article/10.3389/feart.2017.00038/full |
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