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<p><strong>Abstract.</strong> Many mountainous regions depend on seasonal snowfall for their water resources. Current methods of predicting the availability of water resources rely on long-term relationships between stream discharge and snowpack monitoring at isolated locations, which are less reliable during abnormal snow years. Ground-penetrating radar (GPR) has been shown to be an effective tool for measuring snow water equivalent (SWE) because of the close relationship between snow densitydoi:10.5194/tc-11-2997-2017 fatcat:wiuewmjqcvehnjk4f4uzi7p4i4