Between the late 19th and early 21st century, in the Alps the average air temperature has increased by about 2 °C, more than twice the increase in temperature in the northern hemisphere, of 0.8 °C. In the same period, precipitation showed a tendency towards an increase in the northern part of the Alps, and a tendency towards a decrease in the southern sector of the Alps.
Since the end of the Little Ice Age (about 1850), glaciers in the ...
Different approaches have been proposed to model landslide and erosion processes separately. Only a few attempts have been made to model landslide and erosion jointly. Some models consider the effects of landslides on sediment yield and transport. In other cases, landslides and erosion processes are components of a landscape evolution model. However, existing models do not describe jointly the triggering mechanisms of landslide and erosion ...
The ADAPT project, co-funded by the Interreg Italy-France Maritime Program 2014-2020, aims to adapt the Italian and French cities of the Upper Tyrrhenian to the consequences of climate change, with particular reference to the urban flash floods caused by intense meteorological ...
The 3DA software is a new procedure that allows retrieving in near-real-time 3D surface deformation models starting from data acquired via robotized total stations or others system that acquire the surface displacements. The measurements are first pre-processed and then implemented on 3D maps that include vector arrows representative of the intensities and of the real directions of motion in a given system of coordinates. The 3D surface ...
The service analyzes the climate change impact on the main hydro-meteorological variables involved in the hydrological cycle and, in particular, on extreme events of rainfall and discharge (droughts and floods). The service allows to evaluate the combined effects of natural and human processes related to climate change on surface runoff and groundwater, analyzing the possible consequences of such effects on the strategic water ...
A Deep-seated Gravitational Slope Deformation (DGSD) affects the south-west flank of mount Ganderberg (Moso in Passiria – BZ). The continuous displacements of the landslide induce secondary hazardous phenomena. A 800.000 m3 rock slab shows signs of incipient movement; a detachment could create a natural barrier on the river ...
