Persistent snow cover area in the Alps

These maps show the area that remained covered by snow from May 01 to Sep 01 over the past three years. It was computed from Theia Sentinel-2 snow products at 20 m resolution to capture the smallest snow patches.

 

Persistent snow cover area from May 01 to Sep 01. Each dot corresponds to the total area within a region of 20 km by 20 km, i.e. the aggregation of 1 million pixels.

In average there are about 1300 km2 (Lake Geneva: 680 km2) which remain snow-covered until September (less than 1% of the Alps, depending on the definition of the Alps). The persistent snow cover area was highest in 2018, reflecting the exceptional snow accumulation in west Europe mountains this year.

The spatial distribution of the persistent snow is stable from one year to another. In fact, it is mostly found on glacier, as shown here over the Bernina range near St Moritz for 2018.

Persistent snow map and Randolph Glacier inventory 6.0

This is expected: in places where the snow cover does not melt before the end of the summer, the snow mass will increase and start to flow, forming a glacier.

For the next Snow & Ice Copernicus service, the European Environmental Agency requested the distribution of a map indicating the permanent snow line (area) for each year. The algorithm to compute this layer called « PSL » is straightforward (see the script in the LIS repo). The PSL is given by the pixels which have a snow cover probability equal to one over a hydrological year, i.e. pixels which were always detected as snow or cloud/no data. Because the snow detection can fail during the winter season due to shadows in steep slopes, and also to save CPU time, we reduced the period of computation to May 01 – Sep 01 instead of the entire hydrological year.

Plus d'actualités

BIOMASS, the third launched satellite mission designed at CESBIO !

After SMOS in 2009, and VENµS in 2017, the CESBIO Laboratory is very proud to see its third proposed mission, Biomass, reach orbit. As always, it has been a long journey from the idea, at the beginning of the century, to the selection in 2013 as the seventh Earth Explorer Mission by ESA, to the […]

Sentinel-2 reveals the surface deformation after the 2025 Myanmar earthquake

Sentinel-2 captured several clear-sky images of Myanmar before and after the 28 March 2025 earthquake. The animation below shows a 5-day apart sequence of images captured by Sentinel-2B and Sentinel-2C (10 m resolution) near the epicenter located close to Mandalay. The surface slip due to the earthquake follows the Sagaing Fault, a major fault in […]

Evolution de l’altitude de la ligne de neige au cours des 41 dernières années dans le bassin versant du Vénéon (Oisans)

Pour contribuer à caractériser les conditions hydrométéorologiques lors de la crue torrentielle qui a frappé la Bérarde en juin, j’ai analysé une nouvelle série de cartes d’enneigement qui couvre la période 1984-2024 [1]. Grâce à la profondeur temporelle de cette série, on constate que l’altitude de la ligne de neige dans le bassin versant du […]

Rechercher