Semi-arid and arid cities are growing rapidly, often in river basins where water is already overallocated (Sabo et al., 2010). Previous strategies to increase water supply through transbasin imports have become infeasible, so cities have turned to demand management strategies such as efficiency and conservation in municipal outdoor use (Gleick, 2010;Gonzales & Ajami, 2017;Quesnel & Ajami, 2017). Meanwhile, increased urban growth not only stresses water supply systems, but also directly and dramatically alters urban streamflow. While much attention has focused on urban peak flows, alterations to urban baseflow can have magnified ecological consequences in streams with little baseflow under natural conditions (Rolls et al., 2012;Strange et al., 1999). Impervious surfaces alone do not explain changes in urban baseflow (Hopkins et al., 2015). Post-development baseflow has the potential to rise, fall, or remain consistent when compared to pre-development observations (Bhaskar, Beesley, et al., 2016). Potential urban causes of rising baseflow include wastewater effluent outfalls (Dennehy et al., 1993; Townsend-Small et al., 2013), channel deepening and riparian