“…Urban streams experience increases in low flows when inputs from leaky water supply pipes and sewers migrate to the stream between storm events but also experience decreases because impervious surfaces reduce infiltration, the water table level, and therefore rates of groundwater flow entering the stream (Bhaskar et al, 2016). While the extent of urban impervious surfaces is an important control on watershed hydrology, the hydrologic connectivity of these surfaces to stream networks through constructed drainage channels and storm sewers also controls peak discharge and runoff volume (Alley & Veenhuis, 1983;Bell et al, 2016;Dewals et al, 2012;Shields & Tague, 2014;Shuster et al, 2005;Walsh et al, 2005;Walsh & Kunapo, 2009). These drainage networks cause runoff, rich in nutrients like nitrogen (N), to bypass biologically active zones in both the terrestrial and riparian environments, which limits the ability of urban ecosystems to remove or retain excess nutrients that enter the watershed by atmospheric deposition, imported food (subsequently released as wastewater), and applied fertilizer (Bernhardt et al, 2008;Duncan et al, 2013;Groffman et al, 2004;Hatt et al, 2004;Kaushal & Belt, 2012).…”