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Lienz Dolomites

Lienzer Dolomiten

Wed 25 Mar

Day Risk Profile

Low
below 2200m
Moderate
above 2200m

Avalanche Problems

Above 2200 m

Moderate (2) Dry avalanches · all day
Dry snow level 2 Persistent weak layers Slab 2
N, NE, E, W, NW
above 2200m
Medium Few Poor
GM.6 GM.7
Field notes

Persistent 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 are very challenging to recognise. 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 and shooting cracks are typical when present, but you can have a serious weak layer with no warning signs at the surface. Knowledge of how the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has evolved is essential. SLF's travel advice is direct: travel conservatively, avoid terrain where the consequences of being caught are large, and treat the history of weather and snow as more important than what you can see today. Read the full bulletin.

Source: SLF Avalanche Bulletin Interpretation Guide

Avalanche Activity

Weakly bonded old snow requires caution.

Single winter sport participants can release avalanches in some places. These can in some cases be triggered in near-surface layers. Caution is to be exercised in particular on very steep northwest, north and northeast facing slopes above approximately 2200 m, as well as on very steep west and east facing slopes above approximately 2500 m, in isolated cases also on very steep southeast, south and southwest facing slopes in Areas above approximately 3000 m (particularly glaciated areas).EAWS glossary. Mostly avalanches are medium-sized. Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are to be found 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 and adjacent to ridgelines. They are difficult to recognise. Isolated 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 can indicate the danger. Additionally in isolated cases avalanches can be triggered in near-ground layers. The avalanche prone locations are to be found in particular on very steep west, north and east facing slopes above approximately 2200 m. Such avalanche prone locations are rare but are barely recognisable. Especially transitions from a shallow to a deep Snow deposited on the ground in a multiplicity of layers.EAWS glossary are unfavourable. As a consequence of warming during the day and the solar radiation, the likelihood of moist avalanches being released will increase a little on very steep sunny slopes.

Outlook

Increasing avalanche danger

26 March 2026

Increase in avalanche danger as a consequence of new snow and wind.

Snowpack & Weather

Snowpack
Somewhat older wind slabs are lying on the unfavourable surface of an Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary, especially on very steep northwest, north and northeast facing slopes above approximately 2200 m, also on very steep west and east facing slopes above approximately 2500 m, as well as on very steep southeast, south and southwest facing slopes in Areas above approximately 3000 m (particularly glaciated areas).EAWS glossary. Towards its base, the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is faceted and weak, especially on shady slopes above approximately 2200 m. Steep sunny slopes: Sunshine and high temperatures will give rise to moistening of the snowpack.

Source

ALBINA

Issued

24 Mar 16:00 UTC

Valid until

25 Mar 16:00 UTC

Next update

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