2021
DOI: 10.1080/10106049.2021.1950848
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GIS and MCDMA prioritization based modeling for sub-watershed in Bastora river basin

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Cited by 4 publications
(6 citation statements)
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“…However, the relief parameters recorded a significant increase in their values, with considerable variation among the studied sub-watersheds, highlighting the pronounced influence of these parameters on erosion sensitivity. Consequently, the relief parameters were assigned higher weights in the analysis, taking into account their substantial impact while also acknowledging the significance of the other parameters [19]. Figure 4 depicts the relative weights, and it was observed that basin relief was assigned the highest weight value of 0.308, followed by slope (0.154) and relief ratio (0.103).…”
Section: Criterion Weightage For Mcdamentioning
confidence: 99%
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“…However, the relief parameters recorded a significant increase in their values, with considerable variation among the studied sub-watersheds, highlighting the pronounced influence of these parameters on erosion sensitivity. Consequently, the relief parameters were assigned higher weights in the analysis, taking into account their substantial impact while also acknowledging the significance of the other parameters [19]. Figure 4 depicts the relative weights, and it was observed that basin relief was assigned the highest weight value of 0.308, followed by slope (0.154) and relief ratio (0.103).…”
Section: Criterion Weightage For Mcdamentioning
confidence: 99%
“…The drainage morphometry and parameters of watersheds are responsible for runoff, and thereby erosion phenomena and their characteristics occurring within watersheds [14][15][16]. Morphometric parameters are quantitative representations of watershed geometry and topography [17,18], and they help in understanding a watershed's linear drainage system, its areal pattern, and its relief behavior for the purposes of hydrological engineering [19,20]. These parameters, which include linear, areal, and relief aspects of the watershed, are derived during morphometric analysis of watershed topography [21][22][23][24].…”
Section: Introductionmentioning
confidence: 99%
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“…Watershed morphometric parameters can be used to identify and prioritize critical subwatersheds since they are related to runoff, peak discharge, lag time, soil erosion, and sedimentation risks (Abdeta et al, 2020). Hence, morphometric analysis has recently been used for the prioritization and assessment of watersheds susceptibility to floods and soil erosion especially in the ungauged watersheds and in areas where hydrological simulations are not a viable option (Abdo, 2020; Adnan et al, 2019; Amiri et al, 2019; Arabameri et al, 2018; Bhat et al, 2019; Bhattacharya et al, 2020; Faisal, 2022; Gajbhiye et al, 2014; Haokip et al, 2022; Kulimushi et al, 2021; Mahammad et al, 2022; Nasir et al, 2020; Obeidat et al, 2021; W. Yang et al, 2018).…”
Section: Introductionmentioning
confidence: 99%