2020
DOI: 10.1007/s12517-020-05430-7
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A unified approach for hydrological modeling of arid catchments for flood hazards assessment: case study of wadi Itwad, southwest of Saudi Arabia

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Cited by 9 publications
(5 citation statements)
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“…The example results of surface water modeling are shown in Figure 18. The result shows the typical hydrograph in the arid region, characterized by a steep rising limb (a short time to reach the peak) and rapid recession to zero flow [22]. Figure 18 shows no runoff conditions occurred in November 2019.…”
Section: Hyetograph and Hydrographmentioning
confidence: 96%
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“…The example results of surface water modeling are shown in Figure 18. The result shows the typical hydrograph in the arid region, characterized by a steep rising limb (a short time to reach the peak) and rapid recession to zero flow [22]. Figure 18 shows no runoff conditions occurred in November 2019.…”
Section: Hyetograph and Hydrographmentioning
confidence: 96%
“…The most common storm duration in Saudi Arabia is 3 h [22]. Elfeki et al [23] proposed the appropriate dimensionless cumulative hyetograph for some areas in Saudi Arabia.…”
Section: Rainfall Analysismentioning
confidence: 99%
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“…In Egypt and Saudi Arabia, flash floods are considered to be one of the worst hazards [1][2][3]. There have been numerous flash floods in these locations that have caused substantial social, environmental, and economic losses [5,[7][8][9][10][11][12][13][14]. Floods may transport large sediment loads, endangering wadi settlements and the people who live there [3].…”
Section: Introductionmentioning
confidence: 99%
“…The reason these values are high is that the phi (Ф) index method does to take into consideration the initial abstractions in the basins. Recently, some flash flood studies have been carried out in the study basins, which have focused on the estimation of transmission losses (Elfeki et al, 2014), modelling of flash floods incorporating transmission losses (Noor & Elfeki, 2017), curve number (CN) estimation from field measurements (Farran & Elfeki, 2020a, 2020b, 2020c) estimation of CN from infiltration tests (Elfeki et al, 2020). De Vries and Simmers (2002) stated that despite the numerous studies on the determination of recharge fluxes in arid and semi‐arid regions remain subject to uncertainty.…”
Section: Introductionmentioning
confidence: 99%