“…Groundwater recharge is controlled by a number of factors including precipitation, evapotranspiration, soil type, bedrock geology, climate, vegetation, population among others. Stable isotopes of groundwater provide insight into the seasonal timing and relative efficiency of recharge between seasons (Jasechko et al, 2014(Jasechko et al, , 2017 along with a host of other processes including the degree of evaporation experienced prior to recharge, recharge elevation, surface water-groundwater interaction and connectivity, and paleo-recharge (Siegel and Mandle, 1984;Smith et al, 1992;Squeo et al, 2006;Skrzypek et al, 2015;Follstad Shah et al, 2019;Jasechko, 2019;Nghiem et al, 2019). Thus, understanding spatial patterns in groundwater isotopes greatly aides in characterizing a region's hydrology.…”