- 1Institut de Géosciences de l'Environnement, 54, rue Molière, Saint-Martin d'Heres, France (racovite@gmail.com)
- 2Universty of Strassbourg, School and Observatory of Earth Sciences (EOST)
- 3University Grenoble Alpes, Institut des Sciences de la Terre (ISTerre), France
- 4Department of Geography and Earth Sciences, Aberystwyth University, United Kingdom
- 5Department of Geography, University of Exeter, United Kingdom
- 6University of Bergen, Department of Earth Science
Glacier complexes in the Manaslu region of Nepal Himalaya have been experiencing only moderate mean area losses and geodetic mass balance since the 1970s (~ -0.26 % a-1, -0.17 ± 0.03 m w.e.a−1. Many debris-covered glacier tongues exhibit large amounts of supra-glacial vegetation and stagnating patterns. Here, we investigate these apparent patterns of stagnation of glacier systems in this area, specifically the prevalent vegetation development and the geomorphological characteristics of debris cover tongues. We use remote sensing-derived surface velocities derived from image cross-correlation (RGDyn open-source package) based on Landsat and Sentinel-2 time series combined with high-resolution declassified Corona imagery and Pléiades. Preliminary results indicate ~8 % supra-glacial vegetation coverage at a regional scale and general glacier slowdown with variable movement rates depending on glacier morphology and debris covered characteristics.
How to cite: Racoviteanu, A. E., Fichant, A., Cusicanqui, D., Glasser, N., Millan, R., Harrison, S., and Robson, B. A.: Vegetated debris-covered glaciers and stagnating patterns in the Manaslu region of Nepal Himalaya, EGU General Assembly 2026, Vienna, Austria, 3–8 May 2026, EGU26-14771, https://doi.org/10.5194/egusphere-egu26-14771, 2026.