Avalanche Service Salzburg

Monday 23 February 2026

Published 22 Feb 2026, 18:05:00


Danger level

treeline
Avalanche Problem
Wind slab
Treeline
Persistent weak layer
2000m
Wet snow
1800m


High prone to triggering in wind slabs

The avalanche risk is high above the tree line (4) and considerable below. Individual naturally triggered avalanches are still possible and in many places medium and sometimes large slab avalanches can easily be triggered by individuals (even from a distance). All aspects are affected, but increasingly north and east-facing steep terrain. Danger areas are not easy to recognise everywhere, which is why caution and a very defensive choice of route is still advised. In low and medium altitudes, spontaneous wet loose snow avalanches and gliding avalanches are possible.

Snowpack

Abundant new fallen snow, which fell with rising temperatures and was characterised by strong winds, overlaying wind slabs from the previous days, which in turn lay on an unfavourable base of faceted crystals and deep frost. In areas protected from the wind, on shady slopes above about 2000 m and on sunny slopes above 2400 m, surface hoar has also been snowed in in places. Breaks occur primarily between the last snow packs, but can also penetrate through to the coarse-grained old snow foundation under heavy loads. High avalanche activity and very good blasting successes document the unfavourable snow layering. At low and medium altitudes, heat and rainfall put a strain on the snowpack. In some places, the entire snowpack glides on very steep, unstructured terrain.

Tendency

Precipitation will set in again, with rain falling at times up to around 2000 metres on Tuesday. Above that, 20 to 40 cm will fall. The avalanche situation remains tense.


Danger level

treeline
Avalanche Problem
Wind slab
Treeline
Persistent weak layer
Treeline
Wet snow
1800m


Wind slabs are easy to trigger, naturally triggered avalanches are also possible

The avalanche risk is considerable from the tree line upwards and moderate below. Medium to large slab avalanches can be triggered in some places by a single person. Danger areas are located at the transition from little to more snow and generally next to blown-off areas as well as in the entrance areas to gullies and bowls filled with wind slab. Caution should also be exercised at the edge of forests and in forest aisles. In low and medium altitudes, small to medium wet loose snow avalanches and gliding avalanches are possible.

Snowpack

Rainfall has moistened the snowpack up to altitudes of around 2000 metres, at least on the surface, and at lower altitudes it is partially moist down to the ground. At high altitudes, the new snow cover is inhomogeneous and prone to triggering due to repeated wind influences that vary in strength. Breakages are possible, especially between the last layers of drifting snow, but deeper-lying faceted layers in the persistent weak layer or the coarse-grained base of deep rime are also affected. At low and medium altitudes, heat and rainfall put a strain on the snowpack.

Tendency

Heavy precipitation sets in again, with intense rain at times up to around 2000 metres on Tuesday. Above that, there is heavy new fallen snow of 30 to 60 cm (mainly Steinberge/Hochkönig/Tennengebirge). The avalanche situation worsens again.


Danger level

treeline
Avalanche Problem
Wind slab
Treeline
Persistent weak layer
2000m
Wind slab
Treeline


Consistently avoid steep drift snow areas

The avalanche risk is considerable above the tree line and moderate below. The number and extent of avalanche prone locations increase rapidly with altitude, depending on the influence of the wind. Even a single person can trigger a medium-sized slab avalanche in some places. In particular, be careful near the transitions from little to more snow and in the blown-in entrance areas to steep gullies. The fresh wind slab is usually easy to recognise and should be consistently avoided.

Snowpack

The snow surface is strongly characterised by the wind; blown-off broad ridges and crests lie close to fields of drifting snow that are prone to triggering. This bonded snow overlays soft, faceted layers, and in wind-protected, shady areas above around 2000 metres, surface hoar. Fractures occur either in soft layers near the surface or around the crust that forms the transition to the completely built-up old snow foundation.

Tendency

On Tuesday, 10 to 20 cm of new fallen snow with strong north-westerly winds. The avalanche danger increases.