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Sole, Pejo and Rabbi

Sole, Pejo e Rabbi

Sat 20 Dec

Avalanche Problems

Above 2600 m

Low (1) Dry avalanches · all day
Dry snow level 1 Persistent weak layers Slab 1
N, NE, NW
above 2600m
Small Few Poor
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 2400 m

Low (1) Dry avalanches · all day
Dry snow level 1 Wind slab Slab 1
N, NE, E, W, NW
above 2400m
Small Few Poor
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

Low avalanche danger will prevail.

As a consequence of snowfall above approximately 2000 m and the wind, snow drift accumulations formed during the last two days. The wind slabs are mostly shallow and in some cases prone to triggering. These are clearly recognisable. In isolated cases avalanches can be triggered in the weakly bonded old snow. 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 on extremely steep shady slopes above approximately 2600 m. Mostly avalanches are small.

Outlook

Constant avalanche danger

21 December 2025

The avalanche danger will persist.

Snowpack & Weather

Snowpack
Up to 15 cm of snow, and even more in some localities, has fallen since Tuesday above approximately 2000 m. The wind slabs of the last few days remain in some cases prone to triggering in particular on steep shady slopes above approximately 2400 m. Shady slopes above approximately 2600 m: 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 bottom section of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary. In all regions less snow than usual is lying. The snowpack remains subject to considerable local variations.

Source

ALBINA

Issued

19 Dec 16:00 UTC

Valid until

20 Dec 16:00 UTC

Next update

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