2021
DOI: 10.31223/x59w39
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Earthquake-triggered landslide susceptibility in Italy by means of Artificial Neural Network

Abstract: The use of Artificial Neural Network (ANN) approaches has gained a significant role over the last decade in the field of predicting the distribution of effects triggered by natural forcing, this being particularly relevant for the development of adequate risk mitigation strategies. Among the most critical features of these approaches, there are the accurate geolocation of the available data as well as their numerosity and spatial distribution. The use of an ANN has never been tested at a national scale in Ital… Show more

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Cited by 6 publications
(2 citation statements)
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References 107 publications
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“…Another way to elaborate on model performance is to look at confusion plots (see, Amato et al, 2021), where the model accuracy is decoupled for presence and absence data. These are shown in Figure 6, for both RTS and ALD, as well as for the results obtained from the fit, RCV and SCV.…”
Section: Susceptibility Modeling Performancementioning
confidence: 99%
“…Another way to elaborate on model performance is to look at confusion plots (see, Amato et al, 2021), where the model accuracy is decoupled for presence and absence data. These are shown in Figure 6, for both RTS and ALD, as well as for the results obtained from the fit, RCV and SCV.…”
Section: Susceptibility Modeling Performancementioning
confidence: 99%
“…point 1a) ensures that the simulations will include all of the potential sources that could develop into rockfalls and whose runout could concern the railway network (this work does not attempt to account for any anthropogenic mass displacements in the vicinities of the railway track). We favor SU as suitable mapping units for the description of landslide phenomena (Alvioli et al, 2016;Camilo et al, 2017;Schlögel et al, 2018;Bornaetxea et al, 2018;Tanyaş et al, 2019a,b;Jacobs et al, 2020;Amato et al, 2020;Chen et al, 2020;Li and Lan, 2020). More specifically, we adopted SUs instead of a geometric buffer around the track, because rockfall trajectories initiated in a given SU will be bounded within the SU, with reasonable confidence.…”
Section: Identification Of Rockfall Source Areasmentioning
confidence: 99%