2013
DOI: 10.5194/hess-17-3473-2013
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Contribution of directly connected and isolated impervious areas to urban drainage network hydrographs

Abstract: Abstract. This paper addresses the mass balance error observed in runoff hydrographs in urban watersheds by introducing assumptions regarding the contribution of infiltrated rainfall from pervious areas and isolated impervious area (IIA) to the runoff hydrograph. Rainfall infiltrating into pervious areas has been assumed not to contribute to the runoff hydrograph until Hortonian excess rainfall occurs. However, mass balance analysis in an urban watershed indicates that rainfall infiltrated to pervious areas ca… Show more

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Cited by 21 publications
(9 citation statements)
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“…Furthermore, in pervious urban landscapes, hydrological connectivity to impervious areas is important in two senses: (1) runoff from impervious zones that passes over pervious land can rapidly increase the rate of saturation and result in quick attenuation of flows; and (2) saturationderived flows that are adjacent to impervious areas have pathways of low resistance that can facilitate rapid transfer of large volumes of water. The role of these zones on overall water balance is uncertain and the subject of continued research, but such dynamics may have a significant impact on small-scale proliferation of stormwater and resultant local flood risk (Seo et al 2013). …”
Section: Surface Runoff Dynamicsmentioning
confidence: 99%
“…Furthermore, in pervious urban landscapes, hydrological connectivity to impervious areas is important in two senses: (1) runoff from impervious zones that passes over pervious land can rapidly increase the rate of saturation and result in quick attenuation of flows; and (2) saturationderived flows that are adjacent to impervious areas have pathways of low resistance that can facilitate rapid transfer of large volumes of water. The role of these zones on overall water balance is uncertain and the subject of continued research, but such dynamics may have a significant impact on small-scale proliferation of stormwater and resultant local flood risk (Seo et al 2013). …”
Section: Surface Runoff Dynamicsmentioning
confidence: 99%
“…In general, pervious surfaces (grass and tree canopy) play an important role in reducing the amount of stormwater runoff; however, once the soil in the catchment reaches saturation, the rainfall water flows horizontally across the land surface. This is an indicator that rainfall has exceeded the soil infiltration capacity, which then will lead to runoff [29]. Further, the pervious areas can be a major contributor to the variability in the runoff hydrograph and are the main cause for long hydrograph tails in urban environments [29].…”
Section: Temporal Variations In Organic Carbon Concentrations In Stormentioning
confidence: 99%
“…This is an indicator that rainfall has exceeded the soil infiltration capacity, which then will lead to runoff [29]. Further, the pervious areas can be a major contributor to the variability in the runoff hydrograph and are the main cause for long hydrograph tails in urban environments [29]. Initially, it takes a longer time for pervious areas to become fully saturated, and only then runoff occurs.…”
Section: Temporal Variations In Organic Carbon Concentrations In Stormentioning
confidence: 99%
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“…For an individual building, road or car park it is possible to measure the proportion of the precipitation that lands on impervious areas which enters the sewer network (Lee and Heaney, 2003). However, the patchwork of green and built-up areas complicates analyses when considering the larger scale (Alberti et al, 2007;Seo et al, 2013).…”
Section: Introductionmentioning
confidence: 99%