Lawinenlagebericht

Západné Tatry

HZS
Auf der Karte ansehen

Lawinengefahr

All elevations· Vormittag
3 · Erheblich
All elevations· Nachmittag
3 · Erheblich
Veraltet — dieser Lagebericht ist 3 years ago abgelaufen. Du siehst vergangene Verhältnisse, nicht den aktuellen Bericht.

Kernpunkte

Watch out for wind-wound slabs. In the afternoon there is a risk of spontaneous avalanches from wet snow.

Lawinenprobleme

  • Wind slab· Vormittag

    • Alle Höhenlagen
    Größe
    3

    Stability: very poor · Frequency: some

  • Wind slab· Nachmittag

    • Alle Höhenlagen
    Größe
    3

    Stability: very poor · Frequency: some

  • Wet snow· Nachmittag

    • Below 1,100 m
    Größe
    2

    Stability: poor · Frequency: some

Avalanche Activity

Watch out for wind-wound slabs. In the afternoon there is a risk of spontaneous avalanches from wet snow.

In the Western, High, western part of the Low Tatras and Mala Fatra there is an increased avalanche danger above the forest border, i.e. the 3rd degree. The main avalanche problem remains wind-blown snow. In recent days, it has transported large amounts of snow to the leeward sides of ridges, places under rock walls and narrow couloirs. Especially dangerous are the exposures of S, SE, SW and E orientation. Especially in these places there are hard wind-beaten slabs in which stresses propagate very well. Loosening of these is already possible with a small additional load, especially on steep slopes. In some cases, medium avalanches, exceptionally large spontaneous avalanches, are possible. In the afternoon, the snow cover becomes heavier due to warming and sunlight and loses its strength, so small to medium-sized spontaneous avalanches from wet snow are possible. Especially sunlit orientations ( SW,SE,SE) are dangerous.

Snowpack Structure

Between 20 and 50 cm of new, mostly powdery snow has fallen in our mountains in the last 48 hours. However, this is very unevenly distributed due to strong winds. The mountain ridges have been blown into hard to icy ground. In narrow troughs and especially in shady orientations and where wind speeds have been lower, more powder snow will be locally piled up. In the valleys there are hard wind-beaten slabs in which stresses propagate very well. Most of the new snow is blown into the forest zone. Here the snow is loose powdery and breaks through to the hardpack. In the afternoon, the snow cover gets wet due to the warming and suddenly loses its strength. When moving, it will break through to the hard ground.

Tendency

As the weather warms up, the avalanche situation will stabilise slightly. Compiled by : Pavel Bet'ko

Bulletin data: Stredisko lavínovej prevencie HZS (via EAWS / avalanche.report)

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