2023
DOI: 10.1016/j.catena.2022.106654
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Testing the performances of different fuzzy overlay methods in GIS-based landslide susceptibility mapping of Udi Province, SE Nigeria

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Cited by 33 publications
(25 citation statements)
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“…It is projected that areas in the research region with the most rainfall will be most susceptible. When it comes to the slope, steeply sloping parts are more prone to landslides than gently sloping areas (Nwazelibe et al 2023). The study's classes with the highest likelihood of landslides occurring are those with slopes greater than 30°.…”
Section: Multicollinearity Testing On the Conditioning Factorsmentioning
confidence: 99%
See 1 more Smart Citation
“…It is projected that areas in the research region with the most rainfall will be most susceptible. When it comes to the slope, steeply sloping parts are more prone to landslides than gently sloping areas (Nwazelibe et al 2023). The study's classes with the highest likelihood of landslides occurring are those with slopes greater than 30°.…”
Section: Multicollinearity Testing On the Conditioning Factorsmentioning
confidence: 99%
“…Natural catastrophes have occurred more frequently and had more severe effects recently as a result of declining environmental quality, climate change, fast population growth, and intensive and unsuitable land-use planning (Saha et al 2021). Landslides, soil erosion, oods, earthquakes, and tsunamis, among others, have an in uence on human populations, resulting in serious injuries and fatalities, damage to residences and infrastructure, nancial loss, and social unrest (Nwazelibe et al 2023;Saha et al 2021;Lee 2018). Soil erosion frequently occurs in conjunction with landslides, and vice versa.…”
Section: Introductionmentioning
confidence: 99%
“…(5) Stream power index (SPI) is another landslide susceptibility factor that should be studied. It is a measure of the erosive power of fowing water at a given point of the topographic surface [30]. When the catchment area and slope increases, the amount of water fowing through the slope and the fow rate of water will also increase, and the fowing water will erode the surrounding slopes in the fow direction.…”
Section: Identifcation and Classifcation Of Conditional Factorsmentioning
confidence: 99%
“…It is a proxy for surface saturation and soil moisture estimation in hilly terrains. TWI utilizes topographic elements of the landscape to determine whether water will flow or accumulate (Nwazelibe et al, 2023). TWI is calculated using the formula, TWI=lnnormalAnormals/tanβ …”
Section: Datasets Preparationmentioning
confidence: 99%