Probabilistic rainfall thresholds for landslide occurrence using a Bayesian approach

Various methods have been proposed in the literature to predict the rainfall conditions that are likely to trigger landslides in a given area. Most of these methods, however, only consider the rainfall events that resulted in landslides and provide deterministic thresholds with a single possible out...

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Published inJournal of Geophysical Research: Earth Surface Vol. 117; no. F4
Main Authors Berti, M., Martina, M. L. V., Franceschini, S., Pignone, S., Simoni, A., Pizziolo, M.
Format Journal Article
LanguageEnglish
Published Washington, DC Blackwell Publishing Ltd 01.12.2012
American Geophysical Union
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Summary:Various methods have been proposed in the literature to predict the rainfall conditions that are likely to trigger landslides in a given area. Most of these methods, however, only consider the rainfall events that resulted in landslides and provide deterministic thresholds with a single possible output (landslide or no‐landslide) for a given input (rainfall conditions). Such a deterministic view is not always suited to landslides. Slope stability, in fact, is not ruled by rainfall alone and failure conditions are commonly achieved with a combination of numerous relevant factors. When different outputs (landslide or no‐landslide) can be obtained for the same input a probabilistic approach is preferable. In this work we propose a new method for evaluating rainfall thresholds based on Bayesian probability. The method is simple, statistically rigorous, and returns a value of landslide probability (from 0 to 1) for each combination of the selected rainfall variables. The proposed approach was applied to the Emilia‐Romagna Region of Italy taking advantage of the historical landslide archive, which includes more than 4000 events for which the date of occurrence is known with daily accuracy. The results show that landsliding in the study area is strongly related to rainfall event parameters (duration, intensity, total rainfall) while antecedent rainfall seems to be less important. The distribution of landslide probability in the rainfall duration‐intensity shows an abrupt increase at certain duration‐intensity values which indicates a radical change of state of the system and suggests the existence of a real physical threshold. Key Points A probabilistic approach is needed to evaluate landslide rainfall thresholds Bayes theorem is suited to this purpose Landslide probability is strongly related to the event rainfall
Bibliography:istex:9C7C695555B085EC5BCC90E73D4F3848D21983F1
ArticleID:2012JF002367
ark:/67375/WNG-JXLZKXFD-6
Tab-delimited Table 1.Tab-delimited Table 2.
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ISSN:0148-0227
2169-9003
2156-2202
2169-9011
DOI:10.1029/2012JF002367