Avalanche forecast

Lechquellen Mountains

LWD Vorarlberg
View on map

Avalanche danger

Above 2,000 m· Morning
2 · Moderate
Below 2,000 m· Morning
1 · Low
Above 1,200 m· Afternoon
3 · Considerable
Below 1,200 m· Afternoon
2 · Moderate
Out of date — this forecast expired 4 years ago. You’re viewing past conditions, not the current bulletin.

Highlights

Wet-snow avalanches on steep sunny slopes during the daytime

Avalanche problems

  • Persistent weak layers

    • All elevations
  • Wet snow

    • All elevations
  • Persistent weak layers

    • All elevations

Weather Synopsis

Tuesday: cloudless skies, light winds, mild. Outstanding visibility. Zero-degree level at 3000 m. At 2000 m: 2 to 7 degrees. Light easterly winds, shifting to southerly.

Tendency

Persistently sunny, very mild. Danger of dry-snow avalanches will gradually decrease. Due to higher temperatures and solar radiation, wet-snow and glide-snow avalanche activity will increase during the course of each day, particularly on very steep sunny slopes.

Avalanche Activity

Wet-snow avalanches on steep sunny slopes during the daytime

Avalanche danger is mostly moderate, in the afternoon in some places it is considerable. Danger zones occur above 2000 m mostly in steep shady terrain. Transitions from shallow to deep snow require caution, e.g. at entries into gullies and bowls. Avalanches can be triggered by large additional loading. Fresh small snowdrift accumulations should be avoided in high-altitude exposed terrain, esp. on shady slopes. A cautious route selection is recommended. Due to higher temperatures and solar radiation, small-to-medium, in isolated cases also large-sized wet-snow and glide-snow avalanches are possible on very steep sunny slopes during the course of the day.

Snowpack Structure

In the upper part of the snowpack there are expansively metamorphosed weak layers. More deeply embedded layers are usually adequately blanketed, seldom triggerable. Most triggerable are transitions from shallow to deep snow, unfortunately not visible to the naked eye. In higher altitude exposed zones, small snowdrift accumulations are prone to triggering. On very steep sunny slopes and at lower altitudes there is a melt-freeze crust in the early morning hours. Elsewhere the snowpack is still powdery. At intermediate altitudes on shady slopes more than anywhere else, surface hoar can be found. Through daytime warming and solar radiation the snowpack forfeits its firmness on steep sunny slopes. Naturally triggered smnall-to-medium wet-snow and glide-snow avalanches have been observed, also some large-sized releases.

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

Regions covered