“…Some of the most notable and early recognized changes that occur due to urbanization include increases in imperviousness (roads, buildings, sidewalks, etc .) (Leopold, ; Alley and Veenhuis, ; Grimmond et al ., ; Shuster et al ., ; Schiff and Benoit, ; Ackerman and Stein, ; Han and Burian, ; LaFontaine et al ., ), corresponding heat island impacts (Oke, ; Arnfield, ; Rizwan et al ., ), alterations to the spatial distribution and type of vegetation (non‐native turf grass) (Small, ; Robbins and Birkenholtz, ; Alig et al ., ; Milesi et al ., ; Pataki et al ., ; Pickett et al ., ; Bijoor et al ., ), construction of storm drainage networks (Graf, ; Hsu et al ., ; Meierdiercks et al ., ), channelization of streams (Mitchell et al ., , ), leaky pipes (Bhaskar and Welty, ), and construction of infrastructure allowing imported water to be transported to urban centers (Mitchell et al ., , ; White and Greer, ). However, most of the hydrologic research in urban systems has focused on the impact of increasing imperviousness on stormwater runoff and flood control (Narayana et al ., ; Bost et al ., ; Kibler et al ., ; Fang and Su, ; Levy et al ., ; Olivera and DeFee, ; Guan et al ., ; Yao et al ., ).…”