Savinja Alps and Carinthia

The current snowpack pattern is uncommon and requires special attention and caution!

New fallen snow in the high alpine regions, weak layers persist.

In particular, even a small additional load can trigger a small avalanche on snowdrift accumulations. A triggered avalanche or an otherwise large Additional load may exceed the load-bearing capacity of the deep hard layers, triggering a deep and widespread (large) avalanche. Such weak layers are particularly abundant in the axis above the forest, but are not excluded elsewhere. Gliding avalanches also occur on steep smooth slopes.

At the end of last week, there was up to 20 cm of New fallen snow above an altitude of around 1400 m. Above 1700 m the snow fell on the hard surface of the old snow cover, below that on a breakable crust or soft ground. A strong nor'easter on Sunday morning built up new small snow drifts which did not connect well with the frozen ground. The old snow cover is made up of layers of bonded snow that have already melted a little. Deep below the surface, the old snow cover contains several weak layers of shreds and coarse grains.

There may be some clouds in the morning, partly clear during the day, with occasional clouds on some peaks and slopes. There will be light to moderate northerly winds. Temperatures will be around -3 °C at 1500 m and -10 °C at 2500 m.

The danger of avalanches will remain similar.