“…Hydrologically, it is well established that increases in impervious cover, coupled with drainage systems in urban areas, create a flashier hydrological regime; for example, a study of nine urban areas dispersed across the United States showed a consistent pattern of increased magnitude and frequency of high flow events associated with urbanisation (Brown et al, 2009). Whilst this trend is well documented in temperate regions, evidence from Puerto Rico, where rivers are naturally flashy due to the precipitation regime and catchment characteristics, indicated that urban river regimes did not differ from naturally forested catchments , highlighting the need for further research in other ecoregions (Hughes et al, 2014b). Urbanisation can also modify the hydrological regime at the other end of the continuum via a reduction in base flows (Wenger et al, 2009), aquatic connectivity (Kaushal and Belt, 2012), and sediment delivery and transport (Taylor and Owens, 2009) resulting in changes to channel morphology (Chin, 2007).…”