Prone to triggering wind slab during the daytime changes.
The avalanche risk is moderate above the tree line and low below. Fresh wind slab is the main problem. Slab avalanches can be triggered in places with a small additional load. This is possible above all in steep terrain adjacent to ridgelines in the north, east and south aspects as well as in gullies and bowls. The number of avalanche prone locations increases during the day changes.
On shady slopes at high altitudes, avalanches can break through to deeper layers in the persistent weak layer and reach medium size.
With sunlight, the new fallen snow detaches itself from the rocky steep terrain as small loose snow avalanches and slides down on the crusted old snowpack.
Snowpack
Fresh snowdrift accumulations form with winds from north-westerly directions. Some of these come to rest on a soft layer of snow and can be prone to triggering. In shady high altitudes, layers of faceted crystals can be found deep in the otherwise compact old snowpack. At medium altitudes, the snowpack is wet towards the ground.
Tendency
Depending on the amount of new snow, the avalanche risk may increase slightly.
Danger level
treeline
Avalanche Problem
Wind slab
Treeline
Be aware of the risk of falling!
The avalanche risk is low. Fresh wind slabs that develop during the daytime changes can be problematic. Occasionally, smaller slab avalanches can be triggered with little additional load in steep terrain adjacent to ridgelines. On shady slopes at high altitudes, deeper weak layers can be disturbed in isolated cases with large additional loads.
Snowpack
Fresh, small snowdrift accumulations form with winds from north-westerly directions. Some of these come to rest on a soft layer of snow and can be prone to triggering. In shady high altitudes, layers of faceted crystals can be found deep in the otherwise compact old snowpack. At medium altitudes, the snowpack is wet towards the ground.
