Boletín de aludes

Lechquellen Mountains

LWD Vorarlberg
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Peligro de aludes

Above 2,600 m· Mañana
2 · Moderado
Below 2,600 m· Mañana
1 · Débil
Above 2,400 m· Tarde
2 · Moderado
Below 2,400 m· Tarde
2 · Moderado
Desactualizado: este boletín caducó 2 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

Often favorable conditions in morning, continuing wet-snow avalanches

Problemas de aludes

  • Persistent weak layers

    • Todas las altitudes
  • Wet snow

    • Todas las altitudes
  • Gliding snow

    • Todas las altitudes
  • Persistent weak layers

    • Todas las altitudes

Weather Forecast

Nocturnal hours: Dry, mild, reduced nocturnal outgoing longwave radiation. Wednesday daytime: Mild foehn conditions, high clouds and Sahara dust will hamper the sunshine. At 2000 m: +9 degrees. Moderate southerly winds, stronger in foehn lanes.

Tendency

Conditions will become less stable, and also cooler, with intermittent showers or thunderstorms in afternoon. Danger of wet-snow avalanches rises during the course of the day slightly. The daily forecasts are at an end for this season. Further reports will be published in case of unusual situations.

Avalanche Activity

Often favorable conditions in morning, continuing wet-snow avalanches

Near-surface layers and small drifts can often be triggered, unleashing a small-to-medium slab avalanche. Frequency and size of danger zones increase with ascending altitude. In case of extended bright intervals, medium-sized loose-snow avalanches are possible, possibly endangering exposed zones. Activities in outlying terrain demand experience in assessing avalanche dangers on-site. Danger rises during the course of each day due to warmth and solar radiation. Isolated glide-snow avalanches are possible. Increasing glide-snow avalanches on smooth grass-covered slopes which previously were bare. Avoid zones below glide cracks.

Snowpack Structure

At high altitudes there are weak layers embedded in the snowpack, esp. on steep shady slopes, they are trigger-prone, as are freshly generated snowdrift accumulations. Despite high nocturnal clouds the outgoing longwave radiation is good, often forming a melt-freeze crust, softening quickly the next morning, causing the snowpack to forfeit its firmness. Because ski areas are closed there is little information about snowpack layering at high altitudes. At low and intermediate altitudes the lower layers of the snowpack are often wet, which reinforces gliding.

Bulletin data: Avalanche Warning Service Vorarlberg (CC BY 4.0)

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