EGU25-3516, updated on 14 Mar 2025
https://doi.org/10.5194/egusphere-egu25-3516
EGU General Assembly 2025
© Author(s) 2025. This work is distributed under
the Creative Commons Attribution 4.0 License.
PICO | Friday, 02 May, 08:39–08:41 (CEST)
 
PICO spot A, PICOA.3
Satellite remote sensing of red algal blooms in the snow of the European Alps 
Marie Dumont1, Léon Roussel1, Simon Gascoin2, Diego Monteiro1, Mathias Bavay3, Pierre Nabat4, Jade Ezzedine5, Mathieu Fructus1, Matthieu Lafaysse1, Samuel Morin4, and Eric Maréchal5
Marie Dumont et al.
  • 1Centre d’Études de la Neige, Université Grenoble Alpes, Université de Toulouse, Météo-France, CNRS, Centre Nationale Recherches Météorologiques (CNRM), Grenoble 38000, France
  • 2Centre d’Études Spatiales de la Biosphère (CESBIO), Université de Toulouse, Toulouse 31000, France
  • 3Institut für Schnee und Lawinenforschung (SLF), Forschungsanstalt für Wald, Schnee und Landschaft (WSL), Davos Dorf 7260, Switzerland
  • 4Centre Nationale Recherches Météorologiques (CNRM), Université de Toulouse, Météo-France, CNRS, Toulouse 31000, France
  • 5Laboratoire de Physiologie Cellulaire et Végétale (LPCV), Université Grenoble Alpes, CNRS, Commissariat á l’Énergie Atomique et aux Énergies Alternatives (CEA), Institut National de la Recherche Agronomique (INRA), Grenoble 38000, France

In the European Alps, snow sometimes takes a blood-like color in late spring due to the presence of snow algal blooms. These blooms decrease snow albedo, accelerating snowmelt and potentially feeding back on snow and glacier decline caused by climate change. In the Alps, so far, only sparse information exists regarding the frequency and location of these blooms. We developed a methodology to identify red snow algal blooms in the European Alps on Sentinel-2 image that enabled to separate red blooms from similarly colored snow due to Saharan dust depositions that occurs frequently in the Alps. The methodology was evaluated using 4600 webcam images. We applied the methodology to 5 years of Sentinel-2 images to generate an atlas of snow algal blooms in the Alps.

The atlas was combined to detailed simulations of the snow and meteorological conditions to identify the drivers of the blooms in the Alps as well as to quantify the maximum contributions of red algal blooms to snow melt. Based on this analysis and on projections on the future snow and meteorological conditions under different emission scenarios, we finally conclude that the occurrences of red snow algal blooms in the European Alps by the end of the century will either stay stable or slightly decrease.

How to cite: Dumont, M., Roussel, L., Gascoin, S., Monteiro, D., Bavay, M., Nabat, P., Ezzedine, J., Fructus, M., Lafaysse, M., Morin, S., and Maréchal, E.: Satellite remote sensing of red algal blooms in the snow of the European Alps , EGU General Assembly 2025, Vienna, Austria, 27 Apr–2 May 2025, EGU25-3516, https://doi.org/10.5194/egusphere-egu25-3516, 2025.