As a result of fresh snow and moderate-velocity winds from varying directions, mostly shallow snowdrift accumulations will be generated in ridgeline zones above all else during the night. These drifts can be easily triggered, especially on NW/N/NE facing slopes, or else glide away naturally. Releases will generally be small-sized.
Snowpack
dp.6: cold, loose snow and wind dp.1: deep persistent weak layer
Particularly along the Slovenian border, 5-10 cm of fresh snowfall is anticipated, locally more. The fresh snowdrift accumulations will be deposited atop an unfavorable old snowpack surface above 1600m, particularly on NW/N/NE facing slopes. The old snowpack is expansively metamorphosed, full of faceted crystals. The snowpack is highly varied, even over small areas. There is too little snow on the ground at all altitudes for this juncture of the season.
Tendency
No significant change in avalanche danger le anticipated
Danger level
2400m
Avalanche Problem
Persistent weak layer
2400m
Wind slab
2400m
Circumvent fresh snowdrifts. Evaluate persistent weak layers with caution
As a result of fresh snow and moderate-velocity winds from varying directions, mostly shallow snowdrift accumulations will be generated during the night in ridgeline zones above all else. These drifts can be easily triggered, especially on NW/N/NE facing slopes, or else glide away naturally. Avalanches can fracture down to more deeply embedded layers inside the snowpack and in isolated cases along t Salzburg border, reach medium size. Size and frequency of danger zones tend to increase with ascending altitude.
Snowpack
dp.6: cold, loose snow and wind dp.1: deep persistent weak layer
Particularly along the Salzburg border, 5-10 cm of fresh snow is anticipated, locally more. The freshly generated snowdrift accumulations will be deposited atop an unfavorable old snowpack surface, particularly on NW/N/SE facing slopes above 2400m. The old snowpack is expansively metamorphosed, full of faceted crystals. The snowpack is highly varied, even over small areas. There is too little snow o the ground at all altitudes for this juncture of the season.
Tendency
No significant change in avalanche danger levels anticipated
Danger level
1800m
Avalanche Problem
Persistent weak layer
1800m
Too little snow on the ground for winter sports widespread. Danger zones in gullies and bowls.
The snowdrift accumulations on steep shady NE/N/NW facing slopes above 1800m can in isolated cases trigger an avalanche usually by large additional loading. Particularly unfavorable are gullies and bowls where hardened layers blanket weakly consolidated old snow. These danger zones occur rather seldom, and are generally small-sized. Apart from the risk of being buried in snow masses, you also need to take the dangers of being swept along and forced to take a fall into consideration.
Snowpack
dp.1: deep persistent weak layer
Snowdrift accumulations cover a weak old snowpack surface on shady slopes above 1800m. The old snowpack is weak, with faceted crystals. The snowpack is highly irregular even over small areas. At all altitudes, there is too little snow on the ground for this juncture of the season.
Tendency
No significant change in avalanche danger levels anticipated
