Abstract

The idea behind any validation scheme in landslide susceptibility studies is to test whether a model calibrated on a certain data can predict an unknown dataset of the same nature (landslide presences/absences and covariates). Almost the entirety of landslide susceptibility studies are validated by subsetting a single dataset into a training and test sets. This dataset usually corresponds either to event-specific or to historical inventories. Very rarely, a multi-temporal inventory is available and, in the few cases where this condition is met, the validation practices involve training a model on a specific landslide inventory, deriving a single predictive equation and validating it on a subsequent landslide inventory. This commonly leads landslide predictive studies, even those with a strong statistical rigor, to neglect the uncertainty estimation in their modeling scheme.In statistics, validation can also be performed via statistical simulations. This means that after fitting a given model, one can generate any number of predictive functions and test their predictive skills on any type and number of unknown datasets. In this work, we take a similar direction and we apply it to model and validate three separate co-seismic inventories, including an uncertainty estimation phase. We mapped these inventories within the same area in Indonesia, for three earthquakes occurred in 2012, 2017 and 2018. Specifically, we build three event-specific Bayesian Generalize Additive Models of the binomial family. From each model we then simulate 1000 predictive realizations over the remaining two inventories, by using a plug-in scheme where all the morphometric covariates are kept fixed and only the ground motion is replaced according to the prediction target. By doing so, we introduce a new analytical tool for near-real-time landslide predictive purposes, which is able to produce a probabilistic model which stands in between the definitions of susceptibility and hazard. In fact, our model is able to accurately estimate “where” and “when” – although not “how frequently” – landslide have occurred by featuring the multitemporal information of the trigger.In our findings, the simulations are quite similar to the fitted models; and the nine combinations we analyse produce excellent performance. This result confirms the assumption that “the past is the key to the future”, as we show that the relative contribution of each variable and their interactions in each probabilistic model remains practically the same across temporal replicates. This information is not trivial because it supports the routines implemented in global near-real-time applications.

Highlights

  • Landslide susceptibility is defined as the probability of a population of landslides to occur over space on the basis of a set of predisposing factors (Brabb, 1984)

  • Being the covariates calculated from a 30 m DEM (SRTM, Jarvis et al, 2008), and the Slope Units (SUs) being on a coarser scale, we further summarized each covariate distribution per SU via its mean and standard deviation (e.g., Amato et al, 2019; Rossi et al, 2010)

  • We discuss the performance for the three reference Generalized Additive Model (GAM) fits and for the six chrono-validated simulation batches (§4.2)

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Summary

Introduction

Landslide susceptibility is defined as the probability of a population of landslides to occur over space on the basis of a set of predisposing factors (Brabb, 1984). Susceptibility usually neglects the contribution to the landslide initiation brought by the main trigger. It does not feature the temporal component which controls the landslide onset. This properties are instead part of the hazard definition, together with the magnitude of the landslide event (Guzzetti et al., 1999, 2005). Model validation is conducted in different ways for models based on historical inventories (e.g., Frattini et al, 2010; Castro Camilo et al, 2017) and event-specific inventories (e.g., Lee et al, 2008; Nowicki et al, 2014)

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