(a) Geology, including geological faults and (b) soil in the target region. 

(a) Geology, including geological faults and (b) soil in the target region. 

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In the face of climate change, the assessment of land transport infrastructure exposure towards adverse climate events is of major importance for Europe's economic prosperity and social wellbeing. Robust and reliable information on the extent of climate change and its projected future impacts on roads and railways are of prime importance for proact...

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In the face of climate change, the assessment of land transport infrastructure exposure towards adverse climate events is of major importance for Europe's economic prosperity and social wellbeing. In this study, a climate index estimating rainfall patterns which trigger landslides in central Europe is analysed until the end of this century and comp...

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... Rainfall-induced soil slope failures most frequent and widespread damaging landslides in the world, causing significant damage to infrastructure and property, endanger human lives, and impact the natural environment (Hong et al., 2005;Baum and Godt, 2010;Cascini et al., 2011;Lee et al., 2014;Igwe et al., 2014;Calvello et al., 2015;Schlögl and Matulla, 2018;Piciullo et al., 2018;Gao et al., 2018;Lu et al., 2020;Nam and Wang, 2020;Sun et al., 2021;Yang et al., 2022;Rahardjo et al., 2005;Ohta et al., 2010;Zhang et al., 2016). Factors such as the intensity, duration, and frequency of rainfall, as well as soil type, topography, and vegetation cover, all contribute to the likelihood of slope failure (Tohari et al., 2007;Sidle and Bogaard, 2016;Wu et al., 2017;Yubonchit et al., 2017;Gonzalez-Ollauri and Mickovski, 2017;Zhang et al., 2019;Picarelli et al., 2020;Wang et al., 2021;Gallage et al., 2021;Jiang et al., 2022a;Lu et al., 2022). ...
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Rainfall-induced soil slope failures are among the most frequent and widespread landslides in the world. The infiltration of water plays a critical role in the instability of slopes under rainfall conditions. By employing the physical models, field monitoring data becomes instrumental for the back analysis of soil parameters, providing critical insights into the mechanisms of slope instability. In this review, the initial section investigates the hydraulic characteristics of unsaturated soils, encompassing the soil-water characteristic curve, permeability function, and their variability nature. Subsequently, a comprehensive overview of infiltration models for unsaturated soil, coupled with their numerical and analytical solutions, is provided. The subsequent section systematically introduces physical model-based Bayesian parameter inference, with a particular emphasis on the formulations of likelihood functions. The exploration then shifts towards investigating the impacts of prior knowledge, likelihood, model structure, and assimilation approach on an unsaturated soil slope monitoring case. Finally, the limitations of the current approaches and future outlooks in this field are presented.
... To assess flood, landslides, and fire hazards, we need to have access to spatial and temporal data to properly model the static and dynamic factors (van Westen et al. 2006). The identified influential factors that have a static nature include topographical aspects (elevation, slope, and aspect), geological factors (rock type, soil depth, and bedrock characteristics), hydrological factors (distance from rivers, drainage density, drainage, and soil moisture), geomorphological aspects (physiographic units and Earth morphologies), and environmental factors (roads and structures) ( Schlögl and Matulla 2018;Hu et al. 2020). Dynamic factors also include rainfall, temperature, humidity, and vegetation characteristics which vary over time and space (Zhu et al. 2014). ...
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Golestan National Park is one of the oldest biosphere reserves exposed to environmental hazards due to growing demand, geographical location of the park, mountainous conditions, and developments in the last five decades. This study aimed to evaluate potential environmental hazards using machine-learning techniques. This study applied maximum entropy, random forest, boosted regression tree, generalized additive model, and support vector machine methods to model environmental hazards and evaluated the impact of affecting agents and their area of influence. After data collection and preprocessing, the models were implemented, tuned, and trained, and their accuracies were determined using the “receiver operating characteristic curve”. The results indicate the high importance of climatic and human variables, including rainfall, temperature, presence of shepherds, and villagers for fire hazards, elevation, transit roads, temperature, and rainfall for the formation of floodplains, and elevation, transit roads, rainfall, and topographic wetness index in the occurrence of landslides in the national park. The boosted regression tree model with a “AUC value” of 0.98 for flooding, 0.97 for fire, and 0.93 for landslides hazards, had the best performance. The modeling estimated that, on average, 16.2% of the area of Golestan National Park has a high potential for landslides, 14% has a high potential for fire, and 7.2% has a high potential for flooding. So, results of this study can be applied by land use planners, decision makers, and managers of various organizations to decrease effects of these hazards Golestan National Park (GNP).
... Terrain ruggedness index (TRI) is the mean difference between a central pixel and its surrounding cells and was used here to quantify landscape heterogeneities ( Figure 4h). It is defined as [42]: ...
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In some arid regions, groundwater is the only source of water for human needs, so understanding groundwater potential is essential to ensure its sustainable use. In this study, three machine learning models (Genetic Algorithm for Rule-Set Production (GARP), Quick Unbiased Efficient Statistical Tree (QUEST), and Random Forest (RF)) were applied and verified for spatial prediction of groundwater in a mountain bedrock aquifer in Piranshahr Watershed, Iran. A spring location dataset consisting of 141 springs was prepared by field surveys, and from this three different sample datasets (S1–S3) were randomly generated (70% for training and 30% for validation). A total of 10 groundwater conditioning factors were prepared for modeling, namely slope percent, relative slope position (RSP), plan curvature, altitude, drainage density, slope aspect, topographic wetness index (TWI), terrain ruggedness index (TRI), land use, and lithology. The area under the receiver operating characteristic curve (AUC) and true skill statistic (TSS) were used to evaluate the accuracy of models. The results indicated that all models had excellent goodness-of-fit and predictive performance, but that RF (AUCmean = 0.995, TSSmean = 0.89) and GARP (AUCmean = 0.957, TSSmean = 0.82) outperformed QUEST (AUCmean = 0.949, TSSmean = 0.74). In robustness analysis, RF was slightly more sensitive than GARP and QUEST, making it necessary to consider several random partitioning options for preparing training and validation groups. The outcomes of this study can be useful in the sustainable management of groundwater resources in the study region.
... Where the frequency and intensity of severe rainfall events is supposed to increase, more landslides will be triggered and exposure to landslide risk will rise in these areas (Gariano & Guzzetti, 2016). In general, the impact of changing climate on rapid and shallow slope instabilities is forecasted to become more severe and widespread across Europe throughout the 21st century (Schlögl & Matulla, 2018). ...
... Guha et al. (2015) concluded that at the beginning of the 21 st century Europe's landslide vulnerable territory is expected to face an increased event of landslide frequency, intensity and fatalities. Schlögl and Matulla (2018) also indicated an overall increase in landslides caused by heavy precipitation in the near (2021-2050) and far future (2071-2100) over the central Europe region (Table 2). Overall, projected changes in heavy precipitation will intensify the occurrence of landslides in some parts of Europe with high confidence (IPCC, 2018). ...
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... This paper partly closes this gap by assessing the road network vulnerability of alpine communities to landslide events in the context of rural road networks. Mountain roads, in contrast to lowland areas, are highly vulnerable due a higher probability of climate-driven hazard events and the inherent obstacles of implementing redundant systems Schlögl and Matulla, 2017;Schlögl and Laaha, 2017;Doll 10 et al., 2014;Eisenack et al., 2011). Nevertheless, the relation between infrastructure and communal development in mountain areas is not one-directional, meaning that it is only the former that can impact the latter; instead, the influence is rather two-way (Jaafari et al., 2015). ...
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... The mean difference between a central pixel and its surrounding cells and quantify landscape heterogeneities, which could exert influence on the localisation of the triggering area of shallow landslides ( Różycka et al., 2017;Schlögl and Matulla, 2018). ...
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