Avalanche Service Styria

Tuesday 30 December 2025

Published 29 Dec 2025, 17:03:00


Danger level

treeline
Avalanche Problem
Wind slab
Treeline


Avalanche danger increases above the tree line with new fallen snow and wind

There is a moderate avalanche risk above the tree line. New fallen snow and sometimes stormy north-westerly winds create fresh snowdrift accumulations. Especially behind broad ridges and ridgelines as well as in gullies and bowls, these can be disturbed in places by individuals and triggered as small to medium-sized slab avalanches. The avalanche prone locations are usually easy to recognise if visibility is good. Apere areas are covered by new fallen snow, making it difficult to recognise the risk of injury.

Snowpack

Under the influence of strong winds, 5 - 15 cm of new fallen snow, locally even more, falls on a crusted can form old snowpack. In many places, a built-up transformed surface or surface hoar is covered. The connection between the drift snow layer and the persistent weak layer is poor. On the shady slopes, there are sometimes weak layers of faceted crystals in the old snow foundation. At lower altitudes, the snow often falls on apery ground.

Tendency

It will remain windy and cold on New Year's Eve, with a few centimetres of new fallen snow again along the northern side of the Alps. Watch out for the wind slab problem!


Danger level

treeline
Avalanche Problem
Wind slab
Treeline


Low avalanche danger, fresh avalanche prone locations due to wind slab.

The avalanche danger is generally low. With new fallen snow and sometimes stormy north-westerly winds, fresh snowdrift accumulations are occasionally formed adjacent to the crest, which can be triggered as small ridgelines, crests or summits with little additional load. This is particularly the case behind broad ridges and crests as well as in gullies and bowls.

Snowpack

Under the influence of strong winds, up to 10 cm of new snow falls on a crusted old snowpack. In many places, a built-up transformed surface or surface hoar is covered. The connection between the drifting snow layer and the persistent weak layer is poor. At lower altitudes, the snow often falls on apery ground.

Tendency

It will remain windy and cold on New Year's Eve. The wind slab problem remains predominant!