Showing Wed 17 Dec 2025 Back to today

Upper Engadine and Silvretta

Val Suot

Wed 17 Dec

Avalanche Problems

Low (1) Dry avalanches · all day
Dry snow level 1 Persistent weak layers 1
All aspects
above 2000m
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 the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary can still be released in very isolated cases in particular on extremely steep shady slopes. In addition clearly visible wind slabs formed especially 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. These are small but can in some cases be released easily. They are to be evaluated with care and prudence in very steep terrain. In Areas above approximately 3000 m (particularly glaciated areas).EAWS glossary and in the regions exposed to the foehn wind these Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are more prevalent and the danger is slightly greater. Mostly avalanches are small. Apart from the danger of being buried, restraint should be exercised in particular in view of the danger of avalanches sweeping people along and giving rise to falls.
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

Snowpack & Weather

Snowpack

The snow depths at intermediate and high altitudes are generally below average for the time of year. There is particularly little snow on the southern flank of the Alps. Only in parts of Lower Valais is snow depth roughly in line with the long-term average. On south-facing slopes and generally below 2400 m, the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is mostly wet or crusted.

Along the Main Alpine Ridge and south of there, fresh and drifted snow was deposited at high altitudes on a thin but heavily faceted Snow deposited on the ground in a multiplicity of layers.EAWS glossary on Tuesday. Avalanches are particularly likely to be triggered in these regions.

North of the Main Alpine Ridge, there are pronounced 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 the Snow deposited on the ground in a multiplicity of layers.EAWS glossary, particularly on northern and eastern slopes above approximately 2400 m, but hardly any avalanches have been triggered there by human activity in recent days. At high altitudes, Tuesday’s strong southerly wind has transported some of the old snow, resulting in local snowdrift accumulations.

Weather review for Tuesday

Towards Tuesday morning, precipitation set in on the Main Alpine Ridge and south of there. The snowfall level was at around 1200 m. In other regions, it was mostly cloudy but dry.

Fresh snow

The following amounts had fallen above 1600 m by Tuesday afternoon:

  • Main Alpine Ridge from the Grand St Bernard Pass to the Bernina and south of there: 5 to 15 cm, in western Ticino up to 20 cm
  • elsewhere dry

Temperature

At midday at 2000 m, between +3°C in the north and -2°C in the south

Wind

From southerly directions:

  • strong in northern regions exposed to the foehn wind and generally at high altitudes
  • moderate at high altitudes on the southern flank of the Alps

Weather forecast to Wednesday

Overnight to Wednesday, some snow will continue to fall on the southern flank of the Alps above 1400 m. During the day, it will be mostly cloudy on the eastern part of the northern flank of the Alps, in Grisons and in Ticino, but elsewhere quite sunny.

Fresh snow

Between Tuesday afternoon and Wednesday morning, the following amounts are expected above 1600 m:

  • Main Alpine Ridge from the Grand St Bernard Pass to the Bernina and south of there: 5 to 15 cm
  • elsewhere dry

Overall between Tuesday morning and Wednesday morning above 1600 m:

  • Main Alpine Ridge from Monte Rosa to the Nufenen Pass, western Ticino, Sotto Ceneri: 20 to 30 cm
  • remaining Main Alpine Ridge of the Valais Alps and Main Alpine Ridge from the Nufenen Pass to the Bernina region, other regions of the central part of the southern flank of the Alps: 10 to 20 cm
  • elsewhere dry

Temperature

At midday at 2000 m, around 0°C.

Wind

Rapidly subsiding southerly, light during the day

Outlook to Friday

On Thursday conditions will be very cloudy on the southern flank of the Alps, with sunny conditions elsewhere. Friday will be quite sunny everywhere. In the west, winds will be occasionally moderate and sometimes strong from the southwest, elsewhere light.

Avalanche risk will decrease slowly in the south but will otherwise remain largely unchanged.

Source

SLF

Issued

17 Dec 06:17 UTC

Valid until

17 Dec 16:00 UTC

Next update

17 Dec 16:00 UTC

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