LiDAR assessment of sediment transport in a small, highly erosive alpine catchment
- 1Institut de Physique du Globe de Paris, Planetology and Space Sciences, Paris, France (boukhari@ipgp.fr, lucas@ipgp.fr, jacquemoud@ipgp.fr)
- 2Univ. Grenoble Alpes, INRAE, CNRS, IRD, Grenoble INP, IGE, Grenoble, France (caroline.le-bouteiller@inrae.fr, sebastien.klotz@irstea.fr)
- 3Université Paris-Saclay, Gif-sur-Yvette, France
With rates locally exceeding one centimeter of denudation per year [1,2], i.e., more than 100 t/ha/year, the Durance basin in the French Alps is one of the world’s most heavily eroding areas [3]. A combination of favorable conditions explains this phenomenon, including a very steep topography, sparse vegetation and a particular susceptibility of the Jurassic black marls, also called Terres Noires, to seasonal climatic forcing [4]. The Draix-Bléone observatory uses hydro-sedimentary stations to instrument several of these small, non-anthropized catchments, where hydrological responses to seasonal storms are rapid and intense [5]. The work presented combines the use of LiDAR time series from airborne, UAV and ground measurements, with sediment flux chronicles recorded at the outlet of the Laval catchment, a small steep watershed (0.86 m2), to address questions of upstream/downstream transport modalities. An assessment of the potential of remote sensing methods for attributing the contributions of each critical zone compartment (channel, gullies, landslides, etc.) to the erosive dynamics of this basin and its connectivity is carried out.
References :
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[5] Draix-Bleone Observatory. (2015). Observatoire hydrosédimentaire de montagne Draix-Bléone [Data set]. Irstea. DOI : 10.17180/obs.draix
How to cite: Boukhari, Y., Le Bouteiller, C., Lucas, A., Jacquemoud, S., Klotz, S., and Griffaton, M.: LiDAR assessment of sediment transport in a small, highly erosive alpine catchment, EGU General Assembly 2024, Vienna, Austria, 14–19 Apr 2024, EGU24-17766, https://doi.org/10.5194/egusphere-egu24-17766, 2024.