Avalanche forecast

Západné Tatry

HZS
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Avalanche danger

Above 1,300 m· Morning
2 · Moderate
Below 1,300 m· Morning
1 · Low
Above 1,300 m· Afternoon
3 · Considerable
Below 1,300 m· Afternoon
1 · Low
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Out of date — this forecast expired 5 months ago. You’re viewing past conditions, not the current bulletin.

Highlights

Watch out for wet avalanches on sunny slopes, in the afternoon !

Avalanche problems

  • Wet snow· Morning

    • Above 1,300 m
    Size
    2

    Stability: poor · Frequency: some

  • Wind slab

    • Above 1,800 m
    Size
    2

    Stability: poor · Frequency: some

  • Wet snow· Afternoon

    • Above 1,300 m
    Size
    2

    Stability: very poor · Frequency: some

Avalanche Activity

Watch out for wet avalanches on sunny slopes, in the afternoon !

In the High, Low and West Mountains, an increased avalanche danger, level 3, has been declared. The main avalanche problem is avalanches from wet snow on sunny slopes. Warming temperatures are expected and positive temperatures are also expected at the highest altitudes of the Tatras. On sunny slopes the snow will get wet and lose cohesion. Spontaneous avalanches may occur, especially in the afternoon. The second avalanche problem is wind-blown snow from the last snowfall. More than 30 cm fell, especially on the northern side of the Tatras. The situation has been complicated by the wind, which has created dangerous snow slabs and pillows. Avalanche release is possible on steep slopes, especially with high additional loads.

Snowpack Structure

More than 30 cm of new snow has been added in the last snowfall period. This has different hardnesses depending on whether it has fallen during windless or windy conditions. The critical layer is precisely the interface between the wind-beaten snow and the older felted snow or the hard base of the old hard snow. Layers of unstable square-grained snow are also present in places in the profile beneath the new snow. On sunny slopes the snow becomes waterlogged with tracks its cohesion. Coherent snow cover is found at elevations above 1200 - 1500 m above sea level depending on orientation.

Tendency

with warming rising

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

Regions covered