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Stream water sourcing from high-elevation snowpack inferred from stable isotopes of water: a novel application of d-excess values
About 80 % of the precipitation at the Colorado River's headwaters is snow, and the resulting snowmelt-driven hydrograph is a crucial water source for about 40 million people. Snowmelt from alpine and subalpine snowpack contributes substantially to groundwater recharge and river flow. However, the d
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