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Stubai Alps Central

Stubaier Alpen Mitte

Fri 30 Jan

Day Risk Profile

Moderate
below treeline
Considerable
above treeline

Avalanche Problems

Above treeline

Considerable (3) Dry avalanches · all day
Dry snow level 3 Persistent weak layers Slab 3
N, NE, E, W, NW
below treeline
Medium Some Poor
GM.6 GM.5
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

Below treeline

Considerable (3) Dry avalanches · all day
Dry snow level 3 Persistent weak layers Slab 3
N, NE, E, W, NW
below treeline
Medium Some Poor
GM.6 GM.5
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

Outside marked and open pistes a precarious avalanche situation will prevail.

The fresh snow as well as the widespread wind slabs are lying on top of a weakly bonded Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary in particular on west, north and east facing slopes above the tree line. Avalanches can be released easily and reach medium size. Remotely triggered avalanches are possible. The Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are widespread and are barely recognisable. The number and size of avalanche prone locations will increase with altitude. Caution is to be exercised 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. Field observations and avalanches triggered by explosives confirm a precarious avalanche situation. Caution and restraint are required.

Outlook

Constant avalanche danger

31 January 2026

Hardly any decrease in avalanche danger.

Snowpack & Weather

Snowpack
10 to 20 cm of snow has fallen. As a consequence of southwesterly wind, wind slabs formed on Wednesday. The new snow and wind slabs are lying on top of a weakly bonded Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. 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 old snowpack. This applies especially on wind-protected west, north and east facing slopes.

Source

ALBINA

Issued

29 Jan 16:00 UTC

Valid until

30 Jan 16:00 UTC

Next update

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