2020
DOI: 10.1007/s10346-020-01420-8
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Soil moisture information can improve shallow landslide forecasting using the hydrometeorological threshold approach

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Cited by 92 publications
(71 citation statements)
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“…Antecedent water content, soil saturation, and pore pressure play key roles in landslide instability [25,28,65], and local soil moisture content can be a precursor of landslide instability [66,67]. Even though soil moisture measurements from space are still limited in resolution and depth, satellite soil moisture information may help constrain the nowcast [68].…”
Section: Spatial Temporal Lag Note Resolution Coverage Resolution Covmentioning
confidence: 99%
“…Antecedent water content, soil saturation, and pore pressure play key roles in landslide instability [25,28,65], and local soil moisture content can be a precursor of landslide instability [66,67]. Even though soil moisture measurements from space are still limited in resolution and depth, satellite soil moisture information may help constrain the nowcast [68].…”
Section: Spatial Temporal Lag Note Resolution Coverage Resolution Covmentioning
confidence: 99%
“…Data-driven method for the assessment of the temporal probability of occurrence Shallow landslides triggering occur in consequence of particular rainfall patterns coupled with particular soil hydrological conditions, related in particular to high degree of saturation in superficial soil levels (Lu and Godt 2013;Vasu et al 2016;Bordoni et al 2019). For these reasons, a data-driven model for evaluating the temporal probability of occurrence of shallow landslides in the test-sites (TEMP) was created coupling rainfall factors to soil saturation degree at the beginning of a rainfall and to the soil types, differentiated in terms of materials derived by different bedrocks.…”
Section: Assessment Of the Spatio-temporal Probability Of Occurrence mentioning
confidence: 99%
“…A second approach concerns the use of a physically based method that combines a hydrological and a slope stability model to estimate the response of the hillslope soils towards an input rainfall event (Montgomery and Dietrich 1994;Iverson 2000;Lu and Godt 2013;Montrasio et al 2014;Canli et al 2018;Kang et al 2020). These models are dynamic, allowing to analyze the change in unstable zones across a test-site during a particular rainfall event (Schilirò et al 2015;Zhuang et al 2017).…”
Section: Introductionmentioning
confidence: 99%
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“…In some regions of the world, the soil wetness at the beginning of the triggering rainfall has been proven to play a major role (Bogaard and van Asch, 2002) and therefore to help improve the early warning systems (Guzzetti et al, 2020;Krogli et al, 2018;Marino et al, 2020). Although in previous works in the Baguio area (Philippines) the importance of the antecedent rainfall has been shown to be key to understanding the triggering mechanisms of MORLEs during typhoons (Nolasco-Javier et al, 2015;Nolasco-Javier and Kumar, 2018), no previous work has involved the analysis of soil moisture.…”
mentioning
confidence: 99%