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Grieskogel Mountains

Grieskogelgruppe

Tue 17 Feb

Updated off-schedule

The provider reissued this bulletin at 16 Feb 17:26 UTC, outside the normal publication cycle.

Day Risk Profile

Moderate
below 1800m
High
above 1800m

Avalanche Problems

Above 1800 m

High (4) Dry avalanches · all day
Dry snow level 4 Persistent weak layers Slab 4
N, NE, E, W, NW
above 1800m
Large Many Very poor
GM.1 GM.6
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

Above treeline

High (4) Dry avalanches · all day
Dry snow level 4 Wind slab Slab 4
All aspects
above treeline
Medium Some Very poor
GM.1 GM.6
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

All elevations

High (4) Dry avalanches · all day
Dry snow level 4 New snow Loose 4
All aspects
Medium Few Very poor
GM.1 GM.6
Field notes

Easy to spot - the snow is fresh. Look at recent avalanche activity in similar terrain, and pay attention to how much new snow has fallen in the last three days. Critical loading depends on temperature, wind, and what was on the surface before the storm. SLF advises waiting until the Snow deposited on the ground in a multiplicity of layers.EAWS glossary has had time to bond before committing to steep terrain in fresh snow.

Source: SLF Avalanche Bulletin Interpretation Guide

Avalanche Activity

Outside marked and open pistes a very dangerous avalanche situation will prevail. The danger exists in particular in alpine snow sports terrain.

The fresh snow and the wind slabs that are being formed by the strong westerly wind can be released easily or naturally in all Direction in which a slope faces as indicated by compass direction of the fall line; i.e. a north slope faces in a northerly direction.EAWS glossary 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 to be found also in areas close to the tree line. Remotely triggered avalanches are possible. Avalanches can in some cases penetrate deep layers and reach large size. This applies on west, north and east facing slopes. Caution is to be exercised in particular in Slope facing downwind/ wind sheltered aspect. Snow deposits can attain several times average snow depth.EAWS glossary starting zones that have retained the snow thus far. On very steep slopes small and, in isolated cases, medium-sized loose snow avalanches are possible.

Outlook

Constant avalanche danger

18 February 2026

The conditions are very dangerous for backcountry touring and other off-piste activities. As a consequence of the strong westerly wind more natural avalanches are possible.

Snowpack & Weather

Snowpack
15 to 30 cm of snow has fallen since Sunday. 15 to 20 cm of snow, and even more in some localities, will fall until Wednesday. The wind will be strong to storm force. The fresh snow and in particular the extensive wind slabs will be deposited on 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. In some places various wind slab layers 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. Faceted 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 bottom section of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary.

Source

ALBINA

Issued

16 Feb 17:26 UTC

Valid until

17 Feb 16:00 UTC

Next update

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Schedule

Off-schedule

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