Abstract. A key component for landslide early warning systems
(LEWSs) is constituted by thresholds providing the conditions above which a
landslide can be triggered. Traditionally, thresholds based on rainfall
characteristics have been proposed, but recently, the hydrometeorological
approach, combining rainfall with soil moisture or catchment storage
information, is becoming widespread. Most of the hydrometeorological
thresholds proposed in the literature use the soil moisture from a single
layer (i.e., depth or depth range). On the other hand, multi-layered soil
moisture information can be measured or can be available from reanalysis
projects as well as from hydrological models. Approaches using this
multi-layered information are lacking, perhaps because of the need to
keep the thresholds simple and two-dimensional. In this paper, we propose
principal component analysis (PCA) as an approach for deriving
two-dimensional hydrometeorological thresholds that use multi-layered soil
moisture information. To perform a more objective assessment we also propose
a piecewise linear equation for the identification of the threshold's
shape, which is more flexible than traditional choices (e.g., power law or
bilinear). Comparison of the receiver operating characteristic (ROC) (true skill statistic, TSS) of
thresholds based on single- and multi-layered soil moisture information also
provides a novel tool for identifying the significance of multi-layered
information on landslide triggering in a given region. Results for Sicily
island, considering the ERA5-Land reanalysis soil moisture data (available
at four different depth layers), corroborate the advantages of the
hydrometeorological approach gained in spite of the coarse spatial
resolution and the limited accuracy of reanalysis data. Specifically, the
TSS of traditional precipitation intensity–duration thresholds is equal to
0.5, while those of the proposed hydrometeorological thresholds is
significantly higher (TSS=0.71). For the analyzed region, however,
multi-layered information seems not to be relevant, as performances in terms
of TSS are similar to those obtained with single-layer soil moisture at the
upper depths, namely 0–7 and 7–28 cm, which can imply that in Sicily
landslide phenomena are mainly influenced by soil moisture in most shallow
soil layers.