I achieved my PhD in 2018, focussing on quantifying geomorphic response and sediment transfer in landslide-prone mountainous environments by constraining spatio-temporal sediment dynamics from state-of-the-art geomorphic techniques: UAV-SfM derived 3D topographic reconstructions, and in-situ produced cosmogenic radionuclides.
I am currently a FNRS postdoctoral researcher (chargé de recherche), working on assessing how the impact of stochastic mass movement processes on the CRN-derived denudation rates depends on their magnitude and frequency. I am also interested in exploring the link between sediment connectivity and long term denudation rates.