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Analysing the relationship between rainfalls and landslides to define a mosaic of triggering thresholds for regional-scale warning systems

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Figure

Figure 1. The Tuscany region, subdivided into 25 alert zones (AZ), with landslide inventory laid over the digital elevation modelthe rain gauge distribution laid over the mean annual precipitation map, as averaged from the measures pertaining to the data set used in thiswork (years 2000–2009) (a) and (b).
Figure 2. The rainfall threshold defined for alert zone A1, compared with two alternative thresholds that were discarded because of a largernumber of false alarms (blue dots above the threshold).
Figure 3. Comparison between the rainfall thresholds defined in this study for each Tuscany alert zone and two literature thresholds definedby Rosi et al
Table 3. Contingency table summarizing the validation procedureat regional level; clockwise from the upper left corner, the num-bers represent true positives, false alarms, true negatives and missedalarms.
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