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We present a fully coupled model that allows simulation of the complete urban freshwater cycle including: runoff from paved and impervious areas, flow through the runoff network, overland flow, infiltration through the unsaturated zone, evapotranspiration (at green areas), and groundwater flow in complex, urban geology.
The forced infiltration impacts the local groundwater table with an average rise of up to 69 cm resulting in significant feedback from the groundwater to the runoff system via drains, overland flow and leakage of groundwater to the pipes and canals of the urban runoff network.
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At distinct rainfall thresholds, roads, percent impervious cover and the stormwater drainage network controlled runoff frequency, runoff depth and runoff ratios.
The importance of the effective distribution of runoff in sewer network throughout a detention facility has recently been recognized.
Rare and high intensity rainstorms are observed and can produce surface water runoff through the network of wadis which provide recharge to groundwater aquifers.
Based on its performance in terms of reproducibility of the water balance runoff coefficients, the network was used to forecast the runoff coefficients up to 2020 and it was found that the increase in runoff coefficients is about 1% per year.
The network of runoff stations was sparse giving rise to high uncertainties in the interpolated runoff map with an average relative interpolation error of 15%.
High rill density may be regarded as indicative of frequent and integrated runoff along a drainage network.
Rodriguez-Iturbe and Valdes (1979) presented a probabilistic description of the movement of runoff through the drainage network of the catchment.
In the karst region, surface runoff enters the dense network of subsurface conduits where there is relatively little filtration, biological uptake, or degradation of nutrients or other nonpoint source pollutants (Ryan and Meiman 1996).
In this paper, we identify two types of connectivity: direct connectivity via new channels or gullies, and diffuse connectivity as surface runoff reaches the stream network via overland flow pathways.
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CEO of Professional Science Editing for Scientists @ prosciediting.com