2019
DOI: 10.1007/s10346-019-01279-4
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Preparing first-time slope failures hazard maps: from pixel-based to slope unit-based

Abstract: In this work, we present a novel quantitative geographical information system-based procedure to obtain the magnitude (area) and frequency of medium to large first-time shallow slope failures. The procedure has been set up at the Barcedana Valley, in the Tremp Basin (Eastern Pyrenees). First, pixel-based susceptibility classes were defined using a slope stability index obtained with the physically based model SINMAP. The frequency calculated from the number of firsttime failures recorded during the last 60 yea… Show more

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Cited by 45 publications
(22 citation statements)
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References 68 publications
(97 reference statements)
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“…Thus, we calculated 56 SU maps, corresponding to the possible (a, c) combinations. The values selected were similar to the ones used in previous works [47,55]. Flat areas were excluded from the delineation process by computing a plains map including all areas of the digital elevation model with slope gradient lower than 5 • .…”
Section: Parametric Delineation Of Slope Unitsmentioning
confidence: 99%
See 1 more Smart Citation
“…Thus, we calculated 56 SU maps, corresponding to the possible (a, c) combinations. The values selected were similar to the ones used in previous works [47,55]. Flat areas were excluded from the delineation process by computing a plains map including all areas of the digital elevation model with slope gradient lower than 5 • .…”
Section: Parametric Delineation Of Slope Unitsmentioning
confidence: 99%
“…The optimal values of the input parameters a and c (i.e., the ones corresponding to the optimal ADSU set), were obtained by minimizing Equation (5) to find the best agreement between the mapped ADSUs and the landslide inventory. Although the optimal ADSU set was selected on the basis of the results obtained from Equation ( 5), we also investigated the use of the custom metric developed in [55,56] for comparison. This metric analyzes the differences between the inventoried landslides and the predicted ones (i.e., the mapped ADSUs in this case), in terms of their cumulative frequency size distributions, and is defined as follows:…”
Section: Determination Of Active Deformation Slope Unitsmentioning
confidence: 99%
“…Thus, we calculated 56 SU maps, corresponding to the possible (a, c) combinations. The values selected are similar to the ones used in previous works [47,55]. Flat areas were excluded from the delineation process by computing a plains map including all areas of the DEM with slope gradient lower than 5⁰.…”
Section: Parametric Delineation Of Slope Unitsmentioning
confidence: 99%
“…Although the optimal ADSU set was selected on the basis of the results obtained from Eq. (5), we also investigated the use of the custom metric developed in [55,56] for comparison. This metric analyzes the differences between the inventoried landslides and the predicted ones-the mapped ADSUs in this case, in terms of their cumulated frequency size distributions, and is defined as follows:…”
Section: Determination Of Active Deformation Slope Unitsmentioning
confidence: 99%
“…e main physical models used to evaluate landslides associated with rainfall are Shallow Slope Stability model (SHALSTAB) [11,12], the Stability Index MAPping model (SINMAP) [13,14], and the Transient Rainfall Infiltration and Grid-based Regional Slope Stability model (TRIGRS) [15][16][17][18][19]. e most recognized and widely used models are currently the SINMAP [13,[20][21][22][23][24][25]. e theoretical basis of using the SINMAP model arises from the fact that it is a large-scale slope stability model utilizing the terrain moisture index obtained from the steady-state hydrological model based on grid units that can be quickly and conveniently calculated.…”
Section: Introductionmentioning
confidence: 99%