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Kaiser Mountains - Waidring Alps

Kaisergebirge - Waidringer Alpen

Thu 2 Apr

Day Risk Profile

Low
below treeline
Moderate
above treeline

Avalanche Problems

Above treeline

Moderate (2) Dry avalanches · all day
Dry snow level 2 Wind slab Slab 2
All aspects
above treeline
Medium Some Poor
GM.6 GM.1
Field notes

Look for fresh snow deposits on Slope facing downwind/ wind sheltered aspect. Snow deposits can attain several times average snow depth.EAWS glossary, in Usually a steep, elongated, eroded trench; typically prone to snowdrift accumulation.EAWS glossary and Rounded or elongated concavity; typically tending to accumulate snowdrift.EAWS glossary, and behind ridgelines and abrupt changes in terrain — these are where the wind has loaded the snow into slabs that are easy to trigger. Recent avalanches, shooting cracks under your weight, and Distinctive noise (resembling a “whumpf” sound) occurring when a weak layer beneath a slab collapses. The air of the weak layer is forced outside the snowpack, with the resulting whumpf sound being heard. The sound usually indicates an unstable situation and can be accompanied by surface cracking. A whumpf is a clear avalanche alert.EAWS glossary sounds are clear confirmations of the problem. The safest move is to avoid wind-loaded terrain entirely. NB wind signs alone don't always mean an avalanche problem exists, and the age of drifted snow is hard to judge.

Source: SLF Avalanche Bulletin Interpretation Guide

Avalanche Activity

Wind slabs are to be avoided.

The no longer entirely fresh wind slabs of the last few days can be released by a single winter sport participant. Such Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are to be found in particular in areas close to the tree line and above the tree line. Caution is to be exercised in particular on wind-loaded slopes, as well as in Usually a steep, elongated, eroded trench; typically prone to snowdrift accumulation.EAWS glossary and Rounded or elongated concavity; typically tending to accumulate snowdrift.EAWS glossary, and behind abrupt changes in the terrain. Additionally in very isolated cases avalanches can penetrate near-ground layers of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary and reach medium size, especially on shady slopes at elevated altitudes.

Outlook

Constant avalanche danger

3 April 2026

Wind slabs are to be evaluated with care and prudence.

Snowpack & Weather

Snowpack
The sometimes strong wind has transported the new snow significantly. In some cases the various wind slabs have bonded poorly together. Isolated avalanche prone Snowpack layer in which the crystals are poorly bonded and the layer has the potential to fail. Typical crystals in dry weak layers causing avalanches are : precipitation particles; surface hoar; faceted crystals; hollow crystals; graupel. Generally >1mm in size, loose grains with few bonds Wet weak layers can be formed by all snow crystal/grain types.EAWS glossary exist in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary, especially on shady slopes.

Source

ALBINA

Issued

1 Apr 15:00 UTC

Valid until

2 Apr 15:00 UTC

Next update

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