FOR 581: Coupling of Flow and Deformation Processes for Modelling the Movement of Natural Slopes

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The development of the movement of large hillslopes until failure is the result of complex interactions of hydrological, subsurface-hydraulic and soil-mechanical processes ranging over large space and time scales. As no reliable simulation methods exist today for such purposes, new solutions are suggested which bring together improved process models with coupling, averaging and upscaling methods while combining deterministical and stochastical approaches to take the complexity of the processes as well as the available data on the different scales into account.