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Titlebook: Engineering Geology for Society and Territory - Volume 1; Climate Change and E Giorgio Lollino,Andrea Manconi,Marta Chiarle Conference proc

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Preliminary Study to Define a Distributed Hydrogeological Model Based on Snow Melt for Groundwater Rto evaluate the groundwater recharge deriving from snow melt process in a mountain basin. An experimental meteorological station was installed by DIATI of Politecnico di Torino in Mascognaz (Ayas) in the Aosta Valley, as part of a project with the Regional government. It is equipped with advanced se
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Seasonal Hydrochemical Changes of Water from Alluvium Aquifers: Drean-Annaba Aquifer Case Study (NE e observed modification, but dryness that the country knew during the last two decades has highly contributed to the water quality changes. During this period, irregularities in the distribution of rainfalls, in time and space, have been observed. As a result, a periodicity in hydrochemical changes
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Assessing Climate Change Risks Under Uncertain Conditions,ycle variables, to the uncertainties in regional climate response, to the uncertainties in the hydrological and/or ecosystem models themselves. Precipitation data used to validate the models, on the other hand, are also affected by severe uncertainties, especially in mountain regions. This leads to
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Response of Alpine Glaciers in North-Western Italian Alps to Different Climate Change Scenariosame year) spring temperature and precipitation conditions. A linear regressive model based on these four climatic variables explains up to 93 % of the variance. When employed for out-of-sample projections, the empirical model displays high prediction skill, and it is thus used to estimate the averag
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Effects of Dust Deposition on Glacier Ablation and Runoff at the Pascua-Lama Mining Project, Chile a a thicker cover increasingly acts as thermal insulation, thus reducing ice ablation and increasing the glacier’s longevity. Data from literature indicate that at less than 1 mm dust thickness ablation rates peak, resulting in ablation increases between 20 and 400 %. Field ablation tests and numeric
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