Glacierized headwater streams as aquifer recharge corridors, subarctic Alaska

Abstract Arctic river discharge has increased in recent decades although sources and mechanisms remain debated. Abundant literature documents permafrost thaw and mountain glacier shrinkage over the past decades. Here we link glacier runoff to aquifer recharge via a losing headwater stream in subarct...

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Bibliographic Details
Main Authors: A. K. Liljedahl, A. Gädeke, S. O'Neel, T. A. Gatesman, T. A. Douglas
Format: Article
Language:English
Published: Wiley 2017-07-01
Series:Geophysical Research Letters
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Online Access:https://doi.org/10.1002/2017GL073834
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