Multitemporal Analysis of Slow-Moving Landslides and Channel Dynamics through Integrated Remote Sensing and In Situ Techniques

The relationships between hillslope and fluvial processes were studied in a mountainous area of the Northern Apennines (Italy) where intermittent landslide activity has interacted for a long time with river morphodynamics. The aim of the study was to analyse such relationships in two study sites of the Scoltenna catchment. The sites were analysed in detail and monitored through time. A long-term analysis was carried out based on multitemporal photointerpretation of aerial photos. Slope morphological changes and land use modifications since 1954 were detected and compared with the evolution of the channel morphology. A short-term analysis was also performed based on two monitoring campaigns accomplished in 2021 and 2022 in order to detect possible slope displacements and channel-bed-level changes. The techniques used are global navigation satellite systems and drone photogrammetry accompanied by geomorphological surveys and mapping. The multitemporal data collected allowed us to characterise slope surface deformations and quantify morphological changes. The combination of various techniques of remote and proximal sensing proved to be a useful tool for the analysis of the surface deformations and for the investigation of the interaction between slope and fluvial dynamics, showing the important role of fluvial processes in the remobilisation of the landslide toe causing the displacement of a significant volume of sediment into the stream

River widening in mountain and foothill areas during floods: Insights from a meta-analysis of 51 European Rivers

River widening, defined as a lateral expansion of the channel, is a critical process that maintains fluvial ecosystems and is part of the regular functioning of rivers. However, in areas with high population density, channel widening can cause damage during floods. Therefore, for effective flood risk management it is essential to identify river reaches where abrupt channel widening may occur. Despite numerous efforts to predict channel widening, most studies have been limited to single rivers and single flood events, which may not be representative of other conditions. Moreover, a multi-catchment scale approach that covers various settings and flood magnitudes has been lacking. In this study, we fill this gap by compiling a large database comprising 1564 river reaches in several mountain regions in Europe affected by floods of varying magnitudes in the last six decades. By applying a meta-analysis, we aimed to identify the types of floods responsible for more extensive widening, the river reach types where intense widening is more likely to occur, and the hydraulic and morphological variables that explain widening and can aid in predicting widening. Our analysis revealed seven groups of reaches with significantly different responses to floods regarding width ratios (i.e., the ratio between channel width after and before a flood). Among these groups, the river reaches located in the Mediterranean region and affected by extreme floods triggered by short and intense precipitation events showed significantly larger widening than other river reaches in other regions. Additionally, the meta-analysis confirmed valley confinement as a critical morphological variable that controls channel widening but showed that it is not the only controlling factor. We proposed new statistical models to identify river reaches prone to widening, estimate potential channel width after a flood, and compute upper bound width ratios. These findings can inform flood hazard evaluations and the design of mitigation measures

Analisi Geomorfologica dei sistemi bacino-conoide dell’Appennino campano: scenari di suscettibilità alluvionale

Basin-fan systems are very dynamic environments in which erosion, transfer and depositional processes are strictly interconnected. In 1996, NRC introduced the term “alluvial fan flooding” to indicate a particular type of flood that occurs only on alluvial fans. The intensity of the flood depends on the flow processes, which can range from water-flood to debris flow (Wells & Harvey, 1987; Costa, 1988). Differentiation between these processes is essentially dependent on the relative concentration of the water and solid components (Costa, 1988; Blair & McPherson, 1994a,b). The increase in the relative proportion of sediments induces an increase in viscosity and shear strength of the flowing mixture. As a consequence, flows on fans may be characterized by different velocities, types of transported material and depositional behavior. This leads to deposits with different size and sedimentary facies and to fans with different slope and morphology (Blair & McPherson, 1994a). Debris flow fans may be subject to violent surges with high sediment concentration, often carrying large boulders and tree trunks, which can be very destructive and affect any part of a fan surface. They are mainly related to massive depositional processes, resulting in weak stratification, lack of sorting, and to the presence of matrix-supported angular to sub-angular clasts (Blair, 1999a; Sorriso-Valvo et al., 1998). Generally these fans are fed by small and step catchments and are characterized by small dimension and step gradients. Geomorphological evidence of debris flow transport is often represented by the occurrence depositional lobes (Marchi et al., 1993; Wilford et al., 2004; De Scally & Owens, 2004, De Scally et al., 2010). Water flood fans are usually bigger than previous fans and characterized by lower gradients. Their facies features include a crude horizontal stratification with alternating beds of cobble, gravel and sand to fine gravel (Blair & Pherson, 1994a,b, Blair, 1999a; Sorriso Valvo et al., 1998; Sohn et al., 1999; Wilford et al., 2004; De Scally et al., 2010). They presents magnitudes and peak discharges from 5 to 40 times lower than debris flow (Kellerhalls & Church, 1990; Hungr et al., 2001; Wilford et al., 2004). This explains why identification of fans that can be reached by debris flows is important for hazard evaluation because they are a much more destructive phenomenon than fluvial floods. Mitigation of the hazard in debris flow fans requires a very peculiar approach (Jackson, 1987; Jackson et al., 1987; Kellerhals & Church, 1990; Wilford et al., 2004). In last few decades several studies pointed out on the possibility to define statistically significant relationships between morphometrical parameters of the basin-fan system and the main depositional process (Melton, 1965; Pasuto et al., 1992, Marchi et al., 1993; Calvache et al., 1997; Guzzetti et al., 1997; Crosta & Frattini, 2004; De Scally & Owens, et al., 2004; Saito & Oguchi, 2005; De Scally et al., 2010). The present study refers to the geomorphological and morphometric analysis of 102 basin/fan systems, located along the border slopes of the carbonate massifs of Southern Apennines (Matese Mts, Taburno Mts, Caserta Mts, Picentini Mts and Maddalena Mts). These areas are prime spots for urban development and are generally considered to be safer than the valley floors. As a result, villages and towns have been built on alluvial fans which, during intense storms, may be affected by flooding and/or debris flow processes. The main goal is to define the most significant morphometric features of these systems that can be used to classify the fans in terms of transport process (debris flow or water flood). This discrimination may be useful to analyze the susceptibility distribution to alluvial fan flooding in the region. The investigation was carried out by means of a multidisciplinary approach, integrating stratigraphic, morphologic, morphometric, historical and statistical analysis. Particularly, field survey was aimed to find stratigraphic logs and morphological evidences that may be useful to evaluate the main depositional process. In order to investigate the relation between depositional process and the morphometry of the basin/fan sytems, 10 variables were determined for each basin-fan system (basin area, basin length, mean basin inclination, feeder channel length, mean feeder channel inclination, basin relief, Melton index, fan area, fan length and main fan inclination). The values were calculated by building up a DTM (resolution 0f 5m) from the contour lines and the point elevation derived from 1:5,000 topographic maps. It was interpolated with the Regularized Spline method by means of ArcGIS Spatial Analyst. The statistical analysis of these variables was carried out by means of Erre software and elaboration of multivariate techniques (Fisher linear discriminant analysis; Logistic Binomial Regression model; Principal Components Analysis; Cluster analysis). Fisher linear discriminant analysis was applied, using as training data the set represented by the 46 systems whose main type of transport was determined by field survey. In addition, the Logistic Binomial Regression model was analyzed in order to find the simplest and most powerful set of predictor variables. The main result was that the best discrimination between debris flow and water flood processes is achieved by means of only two variables, one for the basin (feeder channel inclination) and one for the fan (fan length). Among the 102 systems studied, 68 were classified as debris flow dominated and 34 as water flood dominated, with a probability of a correct classification higher than 90 %. The results obtained were validated by comparison with field data and the descriptions of historical floods. They allowed to detect where alluvial fan flooding might occur and give information on the different degrees of danger, thus contributing to the knowledge of the susceptibility distribution at a regional scale. Regrettably, urban development in recent decades has failed to take the presence of such alluvial fans into account due to the relatively long return time between floods, with consequent loss of historical memory by the local community. This has served only to increase the territorial vulnerability. The results of this thesis may represent a useful tool for further studies aiming at hazard mapping and civil protection interventions

Is afforestation a driver of change in italian rivers within the Anthropocene era?

International audienc

Is afforestation a driver of change in italian rivers within the Anthropocene era?

International audienc

Multiscale map analysis in alluvial fan flood-prone areas

Several case studies of geomorphological mapping at various scales in order to identify areas prone to alluvial fan flooding are presented in this paper. The selected areas are located in southern Italy and are representative of a geomorphic unit (foothills consisting of coalescent alluvial fans) found throughout the southern Apennines. The medium-scale approach represents the best tool to identify areas susceptible to flooding, using detailed geomorphological mapping of fan systems. It can be considered a preliminary analysis, which provides important information for large areas and identifies zones which need further investigation. Large-scale map analysis may be applied to a single fan and used to distinguish fan portions prone to different degrees of hazard exposure, thus providing accurate information for decision-makers who are called upon to plan hazard management. In both cases, analysis based on detailed geological and geomorphological field surveys is often coupled with remotely sensed data

Modeling the long-term planform evolution of meandering rivers in confined alluvial valleys: Etsch-Adige River, NE Italy

We combine the use of a morphodynamic model for river meander planform evolution with a geological dataset to investigate the influence of external confinements on the long-term evolution of a meandering river flowing in an Alpine valley. The analysis focuses on a 100 km reach of the Adige River, NE Italy, which had several sinuous/meandering sections before being extensively channelized in the 1800s. Geological surveys and historical maps revealed that many sections of the study reach impinge on the borders of the valley during its evolution. Moreover, a marked spatial heterogeneity in floodplain vertical accretion rates likely reflects preferential positions of the river channel in the floodplain. Valley confinements are represented by bedrock outcrops and by alluvial fans created by lateral tributaries, and were extracted from the geological and historical maps to build the computational domain for the meander morphodynamic model. The model predicts the long-term planform evolution of a meandering river based on a linear solution of the 2D De St Venant-Exner differential system and can manage changes in floodplain erodibility. Model applications allow to isolate the effects of valley bedrock and of alluvial fans in constraining the lateral channel migration. Modeled river channel persistence maps are compared with the available geological information. The present work allows further insights into the role of external confinements to river meander belts, which have been conducted so far mostly assuming the channel to evolve in unconfined floodplains. Future research shall incorporate model components for floodplain vertical accretion rates and for the advancement of alluvial fans occurring at the same time scale considered for meander evolution