Landslide Science for a Safer Geoenvironment 2014
DOI: 10.1007/978-3-319-05050-8_78
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Predictive Capability of Deterministic and Statistical Models in Weathered Granite Soil Watershed

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Cited by 3 publications
(2 citation statements)
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“…Lee et al (2012) compared the effects of several of the upstream contributing area estimation methods for wetness index. Many studies have applied steady-state approaches for the prediction of landslides (Acharya et al, 2005;Terhorst and Kreja, 2009;Gomes et al, 2013;Michel et al, 2014;Pradhan et al, 2014). The steady-state approaches are useful for producing spatially distributed slope stability but are limited to the temporal prediction of the slope stability because of the steady-state description of hydrological fluxes.…”
Section: Physical Approachesmentioning
confidence: 99%
“…Lee et al (2012) compared the effects of several of the upstream contributing area estimation methods for wetness index. Many studies have applied steady-state approaches for the prediction of landslides (Acharya et al, 2005;Terhorst and Kreja, 2009;Gomes et al, 2013;Michel et al, 2014;Pradhan et al, 2014). The steady-state approaches are useful for producing spatially distributed slope stability but are limited to the temporal prediction of the slope stability because of the steady-state description of hydrological fluxes.…”
Section: Physical Approachesmentioning
confidence: 99%
“…Deterministic methods, on the other hand, quantify LS based on the physical principles governing slope stability [14,15]. They are pivotal for engineering design and understanding failure mechanisms, utilizing models like TRIGRS [16], SHALSTAB [17], SINMAP [18], and FSLAM [19]. Despite their precision, deterministic approaches are constrained by their requirement for detailed geotechnical or monitoring data and their applicability to largely homogenous slopes and simple landslide scenarios [4,[20][21][22].…”
Section: Introductionmentioning
confidence: 99%