Austria
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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 ... Towards geohazards resilient infrastructure under changing climates
A trend of increasingly frequent intense rainfalls and changing rainfall patterns is causing a relevant number of landslides and floods affecting urban areas and engineering infrastructures such as roads, railways. Recently Transport networks across Europe experienced several failures the reasons of which are still poorly understood.. To improve the current situation, a step change in the way we design reliable and effective defence structures ... Geomorphometry and sediment dynamics in mountain catchments
The aim of the geomorphometric analysis is to derive indices capable of characterizing the spatial variability of specific hydro-geomorphological processes (e.g., sediment connectivity, erosion and deposit). The growing availability of high-resolution topographic data has increased the interest in geomorphometry and its applications. Debris-flow monitoring in instrumented areas and flash-flood documentation are invaluable ways to gather field ... 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 ... Spatially distributed modelling of landslide phenomena
The application of distributed physically based models is possible on relatively small areas, typically hundreds or few thousands of km2. Distributed modelling of slope dynamics requires many sufficiently detailed information. Knowledge of geotechnical parameters and land use, digital terrain models, medium/high resolution cartography, temporal evolution of soil moisture conditions, are ... Long-term Permafrost Monitoring Network
Permafrost is very sensitive to climate change and the risks associated with its degradation affect traffic routes, settlements and infrastructure. Data on the distribution of permafrost are inconsistent and there is no common strategy to tackle this problem. Local administrators should have the means to manage the risks associated with the degradation of the ... 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 ...