Boletín de aludes

Venediger Group South

LWD Tirol
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Peligro de aludes

Above treeline
2 · Moderado
Below treeline
1 · Débil
Desactualizado: este boletín caducó 2 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

Fresh wind slabs represent the main danger. Weak layers in the lower part of the snowpack necessitate caution.

Problemas de aludes

  • Wind slab

    • Above treeline
    Tamaño
    2

    Stability: poor · Frequency: some

  • Persistent weak layers

    • Above 2,200 m
    Tamaño
    2

    Stability: poor · Frequency: few

Snowpack Structure

As a consequence of snowfall and the wind, fresh snow drift accumulations formed during the last few days. In some cases the various wind slabs have bonded poorly together. They are lying on top of a weakly bonded old snowpack in particular on northwest to north to southeast facing aspects. The weather conditions will foster a gradual stabilisation of the snow drift accumulations. The snowpack will be subject to considerable local variations.

Tendency

Fresh wind slabs represent the main danger. Weak layers in the old snowpack necessitate caution.

Avalanche Activity

Fresh wind slabs represent the main danger. Weak layers in the lower part of the snowpack necessitate caution.

Fresh wind slabs can be released by a single winter sport participant in some cases in all aspects above the tree line. The avalanche prone locations are to be found in particular in gullies and bowls, and behind abrupt changes in the terrain. At elevated altitudes the avalanche prone locations will become more prevalent. Whumpfing sounds and the formation of shooting cracks when stepping on the snowpack can indicate the danger. Mostly avalanches are medium-sized. They can in isolated cases penetrate deep layers and reach dangerously large size. In the south the avalanches are mostly smaller. Caution is to be exercised in particular on very steep northwest, north and east facing slopes above approximately 2200 m. On extremely steep slopes small loose snow avalanches are possible as a consequence of solar radiation. On very steep grassy slopes individual gliding avalanches are possible, but they will be mostly small.

Bulletin data: Avalanche Warning Service Tirol, avalanche.report (CC BY 4.0)

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