2008
DOI: 10.1061/(asce)1084-0699(2008)13:7(597)
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Performances of Rainfall-Runoff Models Calibrated over Single and Continuous Storm Flow Events

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Cited by 52 publications
(34 citation statements)
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“…Negative Sr values indicate that the output parameters (runoff depth and peakflow) decrease with increasing input parameters as observed for D imp and N imp . Tan et al (2008) in Singapore also found strong influence of %Imp, W and N imp on peak flow and runoff depth. However, D imp was less important in the Singapore's study because the site was not intensively developed.…”
Section: Sensitivity Analysis Resultsmentioning
confidence: 82%
See 1 more Smart Citation
“…Negative Sr values indicate that the output parameters (runoff depth and peakflow) decrease with increasing input parameters as observed for D imp and N imp . Tan et al (2008) in Singapore also found strong influence of %Imp, W and N imp on peak flow and runoff depth. However, D imp was less important in the Singapore's study because the site was not intensively developed.…”
Section: Sensitivity Analysis Resultsmentioning
confidence: 82%
“…The most widely used urban water quality model is the Storm Water Management Model (SWMM), developed by the Environmental Protection Agency's (EPA). Application and validation of SWMM have been undertaken at different parts of urban catchments around the world (Warwick and Tadepalli 1991;Abustan 1998;Tsihrintzis and Hamid 1998;Barco et al 2008;Temprano et al 2006;Hood et al 2007;Jang et al 2007;Nazahiyah et al 2007;Park et al 2008;Tan et al 2008). However, most of these studies were carried out in the temperate areas which have very different storm characteristic from tropical rainfall.…”
Section: Introductionmentioning
confidence: 99%
“…Even if the effects of the calibration approach (continuous or event-based) are not insignificant for the overall performance of the model (see e.g. Tan et al, 2008), we do not discuss this aspect here for the sake of brevity.…”
Section: Modus Operandimentioning
confidence: 99%
“…Note that basin 1 (B1) is located along the southeast side of basin 2 (B2), B1 is much smaller than B2, and that the total size of both basins is 2285 km 2 as a continuous event. It is easier to analyze the overall shape of the hydrograph, peak flow and time to peak for a single event compared to a continuous event (Tan et al 2008). The simulation was performed using Vflo TM with 100 runs per event in the MCS to produce reliable results.…”
Section: Results Of Rainfall-runoff Simulationmentioning
confidence: 99%