2017
DOI: 10.1007/978-3-319-56487-6_49
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Mapping of Landslide Risks in a Changing Climate – Development of Simplified Methodology

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“…First, landslide probability is determined for non-transient condition and only with respect to knowledge uncertainty. The stability of a slope can be calculated using SLOPE/W, or a similar tool, and the evaluation of the probability of failure using the point estimation method (see for example Rosenblueth, 1975Rosenblueth, , 1981Odén et al, 2017). Knowledge uncertainty is then assessed for the most crucial/selected parameters, in this case undrained shear strength, friction angle, bulk density and level of permeable layer.…”
Section: Submarine Landslide Induced Resuspension (L)mentioning
confidence: 99%
“…First, landslide probability is determined for non-transient condition and only with respect to knowledge uncertainty. The stability of a slope can be calculated using SLOPE/W, or a similar tool, and the evaluation of the probability of failure using the point estimation method (see for example Rosenblueth, 1975Rosenblueth, , 1981Odén et al, 2017). Knowledge uncertainty is then assessed for the most crucial/selected parameters, in this case undrained shear strength, friction angle, bulk density and level of permeable layer.…”
Section: Submarine Landslide Induced Resuspension (L)mentioning
confidence: 99%