Groundwater is Earth's largest reservoir of fresh, liquid water. Accounting for more than 20% of water usage worldwide and 43% of irrigation water (Earman & Dettinger, 2011;Fetter, 2001;Zektser & Everett, 2004), groundwater serves as the primary source of freshwater for over 2 billion people across the globe (Alley et al., 2002;Famiglietti et al., 2011;Gleeson et al., 2012; WWAP, 2015). Its contributions are expected to increase with rising global population and changing climate, as surface water becomes a less reliable resource (FAO, 2005; OECD, 2011; WWAP, 2015). It is estimated that by 2050, 2 billion additional people will need to be fed, increasing demand on agricultural land use for improved rates of food production (OECD, 2011; WWAP, 2015). As climate change continues to alter patterns of drought and regional recharge dynamics, groundwater will continue to establish itself as an increasingly critical component of the water cycle, as groundwater variability directly impacts surface water (