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OʻzbekchaIlm Vrtača tipus
Municipality of Tržič, Sloveenia · 2 180 m üle merepinna
Järgmine lumesadu: Homme, kuni 3,9 cm
Lumi sel nädalal
Laviinioht
Central Karawanks- Värske lumiüle 1800 m · S SW N NW SE NE E W
- Tuulelumiüle 1800 m · N NW NE E W
- Püsivad nõrgad kihidüle 1800 m · N NW NE
The current snowpack pattern is uncommon and requires special attention and caution! en
In particular, even a small additional load can trigger a small avalanche on snowdrift accumulations. A triggered avalanche or an otherwise large Additional load may exceed the load-bearing capacity of the deep hard layers, triggering a deep and widespread (large) avalanche. Such weak layers are particularly abundant in the axis above the forest, but are not excluded elsewhere. Gliding avalanches also occur on steep smooth slopes.
Lumikate
At slightly warmer air temperatures, the snowpack transforms and collapses more quickly. Snow has melted on the highest peaks on sunny slopes, while only the high alpine regions have remained dry.
The snowpack is made up of layers of bonded snow that are already somewhat compacted. The coherence of the layers of blown snow in snowdrift accumulations built up by the southerly wind during the snowfall is weaker.
In the old snow cover, there are several weak layers of faceted snow crystals and sheared grains deep below the surface.
Kehtib kuni R 20:14 · Allikas: ARSO METEO · EAWS ohuskaala
edelast, puhangud 74 km/h
Kastepunkt -2°
Järgmise 6 tunni jooksul langeb
Vähene pilvisus
Päeva pikkus10 h 31 min3 min lühem