Nested Recharge Systems in Mountain Block Hydrology: High-Elevation Snowpack Generates Low-Elevation Overwinter Baseflow in a Rocky Mountain River

Nested Recharge Systems in Mountain Block Hydrology: High-Elevation Snowpack Generates Low-Elevation Overwinter Baseflow in a Rocky Mountain River

The majority of each year′s overwinter baseflow (i.e., winter streamflow) in a third-order eastern slopes tributary is generated from annual melting of high-elevation snowpack which is transmitted through carbonate and siliciclastic aquifers. The Little Elbow River and its tributaries drain a bedroc...

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Bibliographic Details
Main Authors:	Éowyn M. S. Campbell, M. Cathryn Ryan
Format:	Article
Language:	English
Published:	MDPI AG 2021-08-01
Series:	Water
Subjects:	mountain aquifer recharge mountain block hydrology baseflow isotope geochemistry δ<sup>34</sup>S<sub>SO4</sub> δ<sup>18</sup>O<sub>H2O</sub>
Online Access:	https://www.mdpi.com/2073-4441/13/16/2249

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