Showing Tue 30 Dec 2025 Back to today

Maddalene

Maddalene

Tue 30 Dec

Day Risk Profile

Low
below 2400m
Moderate
above 2400m

Avalanche Problems

Above 2600 m

Moderate (2) Dry avalanches · all day
Dry snow level 2 Persistent weak layers Slab 2
N, NE, E, W, NW
above 2600m
Medium Few Fair
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 2400 m

Moderate (2) Dry avalanches · all day
Dry snow level 2 Wind slab Slab 2
All aspects
above 2400m
Small Some Poor
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

Avalanche Activity

The wind slabs represent the main danger.

As a consequence of the strong to storm force northerly wind, fresh snow drift accumulations will form. This applies especially adjacent to ridgelines and 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. The wind slabs are bonding poorly with the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. The wind slabs of Tuesday are prone to triggering 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 approximately 2400 m. The number and size of Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary will increase with altitude. Mostly avalanches are small. In isolated cases avalanches can be triggered in the weakly bonded old snow. Such avalanche prone locations are to be found in particular on extremely steep shady slopes above approximately 2600 m. In very isolated cases avalanches are medium-sized. Even a small avalanche can sweep snow sport participants along and give rise to falls.

Outlook

Constant avalanche danger

31 December 2025

As a consequence of a moderate to strong wind from northerly directions, further wind slabs will form on Wednesday. These represent the main danger.

Snowpack & Weather

Snowpack
The fresh and older wind slabs are lying on soft layers in particular on shady slopes above approximately 2400 m. In particular shady slopes, above approximately 2600 m: 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. Steep south facing slopes: Hardly any snow is lying. The snowpack will be generally subject to considerable local variations. Here only a small amount of snow is lying for the time of year in all altitude zones.

Source

ALBINA

Issued

29 Dec 16:00 UTC

Valid until

30 Dec 16:00 UTC

Next update

—

See this region on the map