The more recent wind slabs can still be released in some cases in particular on very steep shady slopes above approximately 2200 m, especially at transitions into gullies and bowls. The mostly small wind slabs are clearly recognisable to the trained eye. Restraint should be exercised because avalanches can sweep people along and give rise to falls. Avalanches can in very isolated cases penetrate near-ground layers of the snowpack and reach medium size.
Snowpack
dp.6: cold, loose snow and wind dp.7: snow-poor zones in snow-rich surrounding
Only a small amount of snow is lying for the time of year. Snow depths vary greatly, depending on the infuence of the wind. The more recent wind slabs are lying on unfavourable layers in particular on steep shady slopes at high altitudes and in high Alpine regions. Shady slopes: The snowpack consists of faceted crystals. Isolated avalanche prone weak layers exist in the old snowpack. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface.
Tendency
The weather conditions will facilitate a gradual stabilisation of the snow drift accumulations. Further decrease in danger of dry avalanches.
Danger level
Low avalanche danger will prevail.
The old wind slabs are small and can only be released in isolated cases. Individual avalanche prone locations are to be found on extremely steep shady slopes at elevated altitudes, in particular in gullies and bowls. Such avalanche prone locations are rare and are easy to recognise. Restraint should be exercised because avalanches can sweep people along and give rise to falls.
Snowpack
dp.6: cold, loose snow and wind
Only a small amount of snow is lying for the time of year. The snowpack will be subject to considerable local variations. Shady slopes: The snowpack consists of faceted crystals. Steep sunny slopes: As a consequence of mild temperatures and solar radiation a crust formed on the surface.