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Lechtal Alps Central

Lechtaler Alpen Mitte

Sat 14 Feb

Day Risk Profile

Low
below treeline
Considerable
above treeline

Avalanche Problems

Above 2200 m

Considerable (3) Dry avalanches · all day
Dry snow level 3 Wind slab Slab 3
All aspects
above 2200m
Medium Some Poor
GM.1 GM.8
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

Above treeline

Considerable (3) Dry avalanches · all day
Dry snow level 3 Persistent weak layers Slab 3
N, NE, E, W, NW
above treeline
Medium Some Poor
GM.1 GM.8
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

A sometimes treacherous avalanche situation will prevail. Wind slabs and weakly bonded old snow require caution.

Distinct 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 in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary can be released easily by individual winter sport participants especially in little used terrain. Mostly avalanches are medium-sized. Caution is to be exercised in particular on steep west, north and east facing slopes above the tree line. The Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are difficult 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 the formation of shooting cracks when stepping on the Snow deposited on the ground in a multiplicity of layers.EAWS glossary serve as an alarm indicating the danger. Remotely triggered avalanches are possible in isolated cases. As a consequence of the strong to storm force westerly wind, fresh snow drift accumulations formed during the last few days. These are in some cases prone to triggering above approximately 2200 m. The fresh wind slabs are clearly recognisable to the trained eye. The avalanche situation is more favourable in highly frequented off-piste terrain.

Outlook

Constant avalanche danger

15 February 2026

A sometimes treacherous avalanche situation will persist. Weak layers in the old snowpack represent the main danger. <br/> 10 to 15 cm of snow will fall until Sunday. The wind will be light to moderate. The wind slabs of the last few days will be covered with new snow and therefore difficult to recognise.

Snowpack & Weather

Snowpack
Over a wide area 15 to 30 cm of snow, and even more in some localities, has fallen since Wednesday. The westerly wind has transported the new snow significantly. The fresh wind slabs are lying on Transparent, frequently flat crystals forming on the snowpack when moist air settles on the surface. It forms most often during cold, clear, humid nights. Once it is blanketed by fresh fallen snow, surface hoar is one of the most critical weak layer. See also: www.snowcrystals.itEAWS glossary in some places, in particular in places that are protected from the wind above approximately 2200 m. Above the tree line: Distinct 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. This applies in particular on west, north and east facing slopes. Below the tree line: The old snowpack is moist and its surface has a Layer of hard-compacted snow resulting from a melt-freeze process or wind.EAWS glossary that is barely capable of bearing a load.

Source

ALBINA

Issued

13 Feb 16:00 UTC

Valid until

14 Feb 16:00 UTC

Next update

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