As stated in many issues, the climate a leading cause of triggering and evolution of mass movements. Differently from other triggering factors the climatic factors can be well defined for the past and forecasted in the short and medium term. Therefore, the recognition of the climatic trends related to geomorphological and hydrogeological modifications allows for a prevision of landslides and other impacts on human life. The Fourth Assessment Report (AR4) on Climate Change (IPCC) predicts that the global sea level will rise of 60 cm by the year 2100 in response to the warming of the oceans and melting of glaciers. This could have a significant impact on the evolution of the environment if we take into account that coastal areas house approximately 10% of the world population. This paper describes an example of how climate change, and all possible related effects, played a driving role on the triggering and evolution of a huge landslide. The studied area is the coastal slope of the town of Vasto (Abruzzo, Central Italy) recently affected by numerous landslide reactivations. The landslide body extends for 2 km2 from the crown zone (at about 150 m a.s.l.) towards the coastal line. The deep-seated gravitational deformations and large landslides with submarine foots observed on the Vasto coastline are typical of mass movements occurring along the Adriatic coast, in the Plio-Pleistocene sequences represented by clays, sands and conglomerates with continental deposits covers. This study shows that the historical reactivations of the landslide, as well as its scarp retrogression, are related to transients destabilizing factors such as rainfall or snow-melting whereas oldest and deeper mass movements were caused by various eustatic fluctuations in sea level, starting from the emergence of the slope in the middle Pleistocene, where the sub-aerial phase of the transgressive marine succession began. A paleo-morphologic reconstruction of the slope enabled to correlate the numerous instabilities over time to the fluctuations in the level of the Adriatic Sea from the Middle Pleistocene to the present. For a more complete study, it was necessary to reconstruct a "geological-evolutionary model of the slope" that could explain the current stratigraphic features and the actual landsliding framework. The evolutionary model has been useful to understand and explain how the variation in sea level due to climate changes and the simultaneous lifting of the area conditioned the present morphology of the hillside, predisposing the slope to a widespread landsliding. The results of geological-evolutionary model of the slope were validated using a Finite Elements stress-strain analysis carried out by means of the FLAC 6.0 calculation code. The stress-strain numerical simulations show that the first activation of the landslide Vasto would have taken about 200,000 years ago at a rapid rising of sea level. In conclusion, the landslide mass currently observable reflects a phenomenon of instability which was fully activated approximately 200,000 years ago, in correspondence with a phase of high marine station. This instability continued to evolve with local events up to the present day.

The paper reports the results of a slope-atmosphere interaction analysis performed with reference to geo-hydro-mechanical conditions typically observed on the Southern Apennines (Italy). The aim of the analysis is to gain some understanding in the characterisation of climatic variables employed to identify instability thresholds in clay slopes. A seepage analysis was undertaken first, showing that Mediterranean climates can produce significant pore-pressure changes also at depths not usually considered to be affected by atmospheric conditions. Based on the results of the seepage analysis, limit equilibrium analyses were carried out for a 5 m and a 20 m deep landslide, confirming that also deep movements in clay slopes can be related to slope-atmosphere interaction. The characterisation of climatic variables aimed at identifying instability thresholds is finally discussed based on the analyses reported in the paper. The results show that net rainfall cumulated over 2 and 6 months represent suitable climatic variables for the 5 m and the 20 m deep landslide, respectively. These findings suggest that the stability of a clay slope, when referred to shallow movements, is likely to depend on the rainfall infiltrating over a few weeks at least. When deep movements are considered, the stability seems to depend more on the rainfall gradually infiltrating during the most rainy seasons

The data presented in this article are related to the research article described by (Cossu et al., 2018). The data set for this article contains chemical analyses of groundwater and leachate, isotope analysis of groundwater and leachate around a group of landfills located in the municipality of Conversano, close to Bari, the main town of the Apulia Region (Southern Italy). Groundwater samples were collected from eighteen wells. The hydrogeological and chemical study was used to define geochemical features, groundwater and leachate characteristics and to study their potential macroscopic mixing. The land use analysis highlighted quantity and type of used fertilizers permitting to compare these with groundwater in terms of isotopic signature.