CORDIS Project
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This project develops a landscape evolution model to analyze how sediment dynamics influence fluvial incision in postglacial landscapes. It focuses on the European Alps to quantify response times of mountain ranges to deglaciation, aiding in ecosystem management and natural hazard assessment.
Repeated glacial-interglacial cycles during the Quaternary have significantly impacted the topography of many mountain ranges around the world.
Yet, the response of landscape evolution to repeated climate oscillations has not been well quantified.
In recently deglaciated landscapes, the transition from glacial to fluvial/hillslope processes have induced progressive topographic adjustments, and the large amounts of sediments inherited from glacial periods and generated through landsliding of over…
HELMHOLTZ ZENTRUM POTSDAM DEUTSCHES GEOFORSCHUNGSZENTRUM GFZ
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