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Quantifying groundwater‐surface water interactions in a proglacial moraine using heat and solute tracers
Author(s) -
Langston Gregory,
Hayashi Masaki,
Roy James W.
Publication year - 2013
Publication title -
water resources research
Language(s) - English
Resource type - Journals
SCImago Journal Rank - 1.863
H-Index - 217
eISSN - 1944-7973
pISSN - 0043-1397
DOI - 10.1002/wrcr.20372
Subject(s) - groundwater , moraine , hydrology (agriculture) , groundwater flow , hydraulic conductivity , environmental science , surface water , geology , watershed , water balance , inflow , glacier , geomorphology , soil science , aquifer , geotechnical engineering , soil water , environmental engineering , oceanography , machine learning , computer science
Key Points Energy and mass balance methods give consistent estimates of water balance. Mass/energy balance technique is an effective tool for alpine hydrology. Groundwater dominates the water balance of the proglacial tarn.

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