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OʻzbekchaIt-temp fuq Stenar
Municipality of Kranjska Gora, is-Slovenja · 2,501 m 'il fuq mil-livell tal-baħar
Silġ fl-art: 2.0 cm fil-quċċata, 0 cm fil-bażi
Silġ din il-ġimgħa
Periklu ta' valanga
Central Julian Alps- Borra ġdida'il fuq minn 1800 m · S SW N NW SE NE E W
- Pjanċi tar-riħ'il fuq minn 1800 m · N NW NE E W
- Saffi dgħajfa persistenti'il fuq minn 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.
Saff tal-borra
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.
Validu sa Ġim 20:14 · Sors: ARSO METEO · Skala tal-periklu EAWS
punent, buffuri 73 km/h
Punt tan-nida -5°
Nieżla fis-6 sigħat li ġejjin
L-aktar ċar
Dawl tal-jum10 h 31 min3 min iqsar