2011
DOI: 10.1016/j.geomorph.2011.05.015
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Functional soil-landscape modelling to estimate slope stability in a steep Andean mountain forest region

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Cited by 18 publications
(6 citation statements)
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“…This wide range has to be attributed to the very small dataset. Ließ et al (2011) reach an equally high model uncertainty when predicting bulk density using the same dataset. In contrast to this, Ließ (2011) achieved a lower variability in r xy by using a bigger dataset of 315 auger points to predict soil horizon thickness and occurrence probability.…”
Section: Regression Tree and Random Forest Model Performancementioning
confidence: 79%
“…This wide range has to be attributed to the very small dataset. Ließ et al (2011) reach an equally high model uncertainty when predicting bulk density using the same dataset. In contrast to this, Ließ (2011) achieved a lower variability in r xy by using a bigger dataset of 315 auger points to predict soil horizon thickness and occurrence probability.…”
Section: Regression Tree and Random Forest Model Performancementioning
confidence: 79%
“…In a second phase, a statistical classification model, for example logistic regression (LR) (Atkinson and Massari 1998;Ayalew and Yamagishi 2005;Ohlmacher and Davis 2003), discriminant analysis (Adrizzone et al 2002;Carrara 1983) or generalized additive models (Goetz et al 2011;Park and Chi 2008), is applied to discriminate landslide from non-landslide pixels/objects in the multidimensional space of topographic, geological and land use features. Due to the complexity of topographic and geological conditions associated with landslide occurrence, more flexible nonlinear methods such as machine learning algorithms have also been considered, in particular artificial neural networks (Ermini et al 2005;Lee et al 2004;Melchiorre et al 2008;Neaupane and Achet 2004;Yilmaz 2010b), support vector machines (SVM) (Ballabio and Sterlacchini 2012;Yao et al 2008;Yilmaz 2010a), Gaussian processes (Gallus 2010) and random forests (RF) (Liess et al 2011;Stumpf and Kerle 2011). Great effort has been placed upon comparing these different approaches both for LS mapping (Brenning 2005) and in a broader context for geomorphological and landform mapping (Brenning 2009;Marmion et al 2008Marmion et al , 2009Nefeslioglu et al 2008;Pradhan and Lee 2010;Yesilnacar and Topal 2005).…”
Section: Introductionmentioning
confidence: 99%
“…The lower probability below 2100 m a.s.l. must be attributed to the higher inclination that supports a higher discharge of surface and subsurface flow and the higher bulk soil density [52]. In contrast, particularly the flat platform-like areas above 2100 m show a much higher probability.…”
Section: Resultsmentioning
confidence: 98%