Slovenia
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Where we should not expect landslides?
Landslide susceptibility is the propensity of a territory to generate landslides.
Many methods are available to determine landslide susceptibility, whereas only a few attempts were made to outline areas not likely to generate landslides i.e., non-susceptible landslide areas. This is surprising, because for planning purposes it is just as important (if not more important) to know where landslides are not expected than to know where landslides ... MUltiHAzard framework for water related risks management
The MUHA project is building upon the idea to address disaster management cycle consisting of preparedness-response-mitigation-rebuild components in the ADRION countries. It will connect the observed and modelled hazards and risks related to the integrated water cycle, by effectively join them with the existing and improved coping capacity developed by national, bilateral and EU Civil Protection ... Connecting European Connectivity Research
Water and sediment connectivity has emerged in recent years as a significant conceptual framework for understanding the transfer of surface water and sediment through landscapes. Connectivity can be seen both as a driver of hydrological and geomorphic processes within a catchment and as an emergent catchment property that is the result of processes acting at different ... Sediment management in Alpine basins
The understanding of the changing equilibrium between sediment supply from upstream and sediment transport capability of a river is important for the success of integrated water resource management. In Alpine river basins, intensive sediment transport processes and sediment continuity have a notable impact on several water management issues posing multiple use conflicts related to hydropower, ecology, flood control ... Hydrometeorological data resources and technologies for effective flash flood forecasting
Flash-floods develop at space and time scales that conventional observation systems for rainfall and river discharge are not able to monitor. Consequently, the atmospheric and hydrological generating mechanisms of flash-floods are poorly understood, leading to highly uncertain forecasts of these ...