Showing Sat 29 Nov 2025 Back to today

Upper Engadine and Silvretta

Zuoz

Sat 29 Nov

Avalanche Problems

Moderate (2+), upper end of the band Dry avalanches · all day
Dry snow level 2 Wind slab + Persistent weak layers 2+
All aspects
above 2200m
The wind slabs of the last few days can still be released in some cases. They are to be evaluated with care and prudence in steep terrain. Additionally avalanches can also be released in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. Mostly the avalanches are medium-sized. Caution is to be exercised in particular on steep shady slopes above approximately 2400 m. Defensive route selection is important.
Field notes

Wind slab

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.

Persistent weak layers

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

Snowpack & Weather

Snowpack

After this week's snowfall, the snow depths in the north and west are well above average for the time of year. In the south, they are below average.

Deeper in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary, especially on shady slopes above approximately 2400 m and in the Areas above approximately 3000 m (particularly glaciated areas).EAWS glossary in general, there are 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 in which avalanches, some large, have been triggered in recent days. In the regions exposed to heavier precipitation in the west and north, these weak layers are now thickly overlaid and are therefore no longer so easily triggered by winter sports participants. However, any avalanches may still become large. In areas with less fresh snow, avalanches are easier to trigger in these weak layers, but will not be quite as large.

With the north to northeasterly wind, snowdrift accumulations have formed at high altitudes over the last two days.

Weather review for Friday

Conditions were mostly sunny and mild in the mountains.

Fresh snow

-

Temperature

At midday at 2000 m, around +1 °C in the north and +3 °C in the south

Wind

Northeasterly

  • moderate and locally strong during the night
  • mostly light during the day
Weather forecast to Saturday

During the night, a little snow will fall in some regions in the north. The snowfall level will rise to 1500 m. During the day it will become increasingly sunny from the west. Conditions will be mostly sunny in the south.

Fresh snow

Northern flank of the Alps from the eastern Bernese Oberland to Liechtenstein and Prättigau: up to 5 cm

Temperature

At midday at 2000 m, around +1 °C

Wind

The wind will shift from north-easterly to westerly and will mostly be light.

Outlook

On Sunday, the east and south will see the last of the bright intervals, while elsewhere it will be very cloudy with light precipitation. A few centimetres of snow will fall in the north by Monday morning. The snowfall level will drop from 1400 to 800 m. On Monday, it will be mostly sunny in the mountains. There will be a light to moderate southwesterly wind.

Avalanche risk will decrease further.

Source

SLF

Issued

28 Nov 15:36 UTC

Valid until

29 Nov 16:00 UTC

Next update

29 Nov 16:00 UTC

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