Wind slab
- Above treeline
Blown snow
Blown snow
The main danger is from blowing snow. The snowpack stability is reduced, especially on slopes and in ravines, where the snow thickness is greater due to snow drifts.
The last snowfall brought strong northerly winds, which blew the snow above the snow line down to the old snow base or to the ground in many places, and built up snowdrift accumulations on the leeward slopes. In some places, these have formed on top of a layer of parachuted graupel, which is a potentially dangerous Weak layer. Locally, the layers of Graupel are 5-10 cm thick, possibly more.
It will be mostly sunny and warmer, around 12 at 1500 m.
The danger of avalanches will remain similar.
Bulletin data: Slovenian Environment Agency (ARSO) (via EAWS / avalanche.report)