Uncertainty in rainfall datasets and landslide inventories is known to have
negative impacts on the assessment of landslide-triggering thresholds. In
this paper, we perform a quantitative analysis of the impacts of uncertain
knowledge of landslide initiation instants on the assessment of rainfall
intensity–duration landslide early warning thresholds. The analysis is based
on a synthetic database of rainfall and landslide information, generated by
coupling a stochastic rainfall generator and a physically based hydrological
and slope stability model, and is therefore error-free in terms of knowledge of
triggering instants. This dataset is then perturbed according to
hypothetical reporting scenarios that allow simulation of possible errors
in landslide-triggering instants as retrieved from historical archives. The
impact of these errors is analysed jointly using different criteria to
single out rainfall events from a continuous series and two typical temporal
aggregations of rainfall (hourly and daily). The analysis shows that the
impacts of the above uncertainty sources can be significant, especially when
errors exceed 1 day or the actual instants follow the erroneous ones.
Errors generally lead to underestimated thresholds, i.e. lower than those
that would be obtained from an error-free dataset. Potentially, the amount
of the underestimation can be enough to induce an excessive number of false
positives, hence limiting possible landslide mitigation benefits. Moreover,
the uncertain knowledge of triggering rainfall limits the possibility to
set up links between thresholds and physio-geographical factors
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