Avalanche forecast

Bregenzerwald Mountains

LWD Vorarlberg
View on map

Avalanche danger

Above 1,800 m
2 · Moderate
Below 1,800 m
1 · Low
Out of date — this forecast expired 4 years ago. You’re viewing past conditions, not the current bulletin.

Highlights

Main danger: snowdrift accumulations prone to triggering; weak old snow at high altitudes.

Avalanche problems

  • Wind slab

    • All elevations
  • Persistent weak layers

    • All elevations

Avalanche Activity

Main danger: snowdrift accumulations prone to triggering; weak old snow at high altitudes.

Fresh snowdrift accumulations are frequently prone to triggering, mostly small. Danger zones occur near to and distant from ridgelines in steep terrain in all aspects and in wind-loaded gullies and bowls, behind abrupt discontinuities in the terrain. One person can trigger an avalanche, usually small-sized. In addition, superficial layers imn gullies and bowls, behind abrupt discontinuities in the terrain, and in transitions from shallow to deep snow can be triggered by large additional loading. Danger zones increase with ascending altitude in size and in frequency. If an avalanche fractures down to more deeply embedded layers in the old snowpack it can grow to medium size. Also, on steep, seldom-tracked shady slopes at high altitudes, deeper layers can be triggered by large additional loading.

Snowpack Structure

Fresh snowfall, strong W/NW winds, new trigger-sensitive snowdrift accumulations in all aspects. Winds have made ridges and crests bare of snow. In many places surface hoar had formed before the precipitation, now blanketed by the fresh snow. On south-facing slopes at high altitudes the fresh snow and drifts often lie atop a melt-freeze crust which is not capable of bearing loads; on north-facing slopes in wind-protected terrain atop soft layers and surface hoar. All in all, the trigger sensitivity of the snowpack has been raised. In ridgeline zone and pass areas, behind abrupt discontinuities in the terrain and in exposed zones, older snowdrift accumulations also occur. They are often inadequately bonded with the old snowpack surface or have weak intermediate layers. At high altitudes, esp. on steep shady slopes, there are often weak layers evident inside the snowpack. These spots are not visible to the naked eye.

Weather Synopsis

Nocturnal hours: gray overcast skies, intermittent light snowfall (snowall level: 800 m). Wednesday: heavily overcast, hardly any sunshine, limited visibility above 1500 m. Light snowfall esp. in Bregenzerwald mountains, Arlberg region, Verwall. At 2000 m: -5 degrees. Strong westerly winds.

Tendency

With increasing snowfall and strong NW winds, avalanche danger will increase significantly over widespread areas.

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

Regions covered