2020
DOI: 10.1016/j.catena.2020.104630
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The influence of the inventory on the determination of the rainfall-induced shallow landslides susceptibility using generalized additive models

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Cited by 67 publications
(30 citation statements)
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“…In any case, a significance of the extreme event cannot be excluded, which is widely documented in the case of surface gravitational phenomena [39,40]. Among the discriminating and statistically significant parameters for the production of landslide movements, there are the slope gradient, which from 5 to 30 • shows an excellent correlation, the agricultural terrain and the geological formation MUS, according to the relevant scientific literature [9,41,42]. The validation procedure allowed, the reliability of the model to be assessed at about 70%, in line with many other studies that used the same or different calculation methods [15,43].…”
Section: Discussionmentioning
confidence: 99%
“…In any case, a significance of the extreme event cannot be excluded, which is widely documented in the case of surface gravitational phenomena [39,40]. Among the discriminating and statistically significant parameters for the production of landslide movements, there are the slope gradient, which from 5 to 30 • shows an excellent correlation, the agricultural terrain and the geological formation MUS, according to the relevant scientific literature [9,41,42]. The validation procedure allowed, the reliability of the model to be assessed at about 70%, in line with many other studies that used the same or different calculation methods [15,43].…”
Section: Discussionmentioning
confidence: 99%
“…As reported by Zhang et al [72], the slope angle is a key factor for slope stability and is one of the most commonly used parameters in LSM studies [73][74][75]. The average slope of the study area, where the slope ranges from 0 • to 76.95 • , is 28.38 • .…”
Section: Landslide-conditioning Factorsmentioning
confidence: 95%
“…As debris flows propagated into the drainage network, they were not included in this analysis. In fact, in this case, the deposits were swept away along the channels and uncertainties occurred in identifying the boundary between debris flows and debris flood deposits [14].…”
Section: Landslide Detachment Transit and Runout Susceptibility (Ldtmentioning
confidence: 99%
“…Shallow landslides usually occur on steep soil-mantled slopes [1][2][3][4][5][6] as a consequence of heavy or intense rainfalls and often may evolve into potentially catastrophic flow-like movements. Slope failures are very common in hilly and mountainous areas due to the combination of several controlling factors such as slope steepness [7][8][9][10], intense or prolonged rainfalls [2,[11][12][13][14], land-use changes [15][16][17][18] and wildfires [19,20]. The consequences of shallow landslides and flow-like phenomena are typically more dangerous in inhabited centers located at the foot of slopes, where the hydrographic network is well developed.…”
Section: Introductionmentioning
confidence: 99%