Showing Thu 14 May 2026 Back to today

Vaud Alps

Bex-Villars

Thu 14 May

Hard-to-read day. Considerable, with new snow and persistent weak layers in play — you can read the surface problem; the buried one sets the consequence.

Day Risk Profile

Considerable

Avalanche Problems

Dry avalanches · all day
Dry snow level 3 New snow + Persistent weak layers 3=
N, NE, E, SE, NW
above 2600m
The fresh snow and in particular the wind slabs that are being formed by the sometimes strong westerly wind are prone to triggering. Single winter sport participants can release avalanches. Dry avalanches can additionally 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 in particular on very steep north facing slopes. These can reach large size. Ski touring calls for experience in the assessment of avalanche danger. The Avalanche Warning Service currently has only a small amount of information that has been collected in the field, so that the avalanche danger should be investigated especially thoroughly in the relevant locality.
Field notes

New snow

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.

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

Fresh snow and wind are forming medium-sized snowdrift accumulations in the west and north, and generally smaller ones elsewhere. Below this, the top section of the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary contains coarse-grained 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, primarily on north- and east-facing slopes at high altitudes.

Weather review for Wednesday

There were cloudy spells overnight in the west and south, while skies were quite clear in the east. It was rather sunny during the day.

Fresh snow

-

Temperature

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

Wind

Light to moderate from westerly directions

Weather forecast until Ascension Day

The night will be rather cloudy. On Ascension Day it will be quite sunny along the Main Alpine Ridge in Upper Valais and in the Gotthard region, while elsewhere it will be very cloudy. Precipitation will be encountered over a wide area. The snowfall level will be between 1300 m in the north and 1800 m in the south.

Fresh snow

Until Ascension Day afternoon, the following amounts will fall above 2000 m:

  • Extreme west of Lower Valais, Vaud and Fribourg Alps: 20 to 30 cm
  • Other regions of Lower Valais and the northern flank of the Alps, Val Bregaglia and the Bernina region: 10 to 20 cm
  • Less elsewhere

Temperature

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

Wind

Southwesterly to westerly

  • Strong on the northern flank of the Alps during the night
  • Elsewhere light to moderate
Outlook

Friday

It will be very cloudy, with around 10 cm of snow falling over a wide area, less in Upper Valais and Ticino. The snowfall level will be around 1300 m. The wind will be mostly light.

The avalanche danger will not change significantly.

Saturday

In the north it will be very cloudy with 10 to 20 cm of snowfall over a wide area. The snowfall level will remain at around 1300 m. Along the Main Alpine Ridge and to the south of it, it will be mostly sunny with a strengthening northerly wind.

There will be a widespread increase in avalanche risk. In Upper Valais and Ticino, it will not change significantly.

Source

SLF

Issued

13 May 15:00 UTC

Valid until

14 May 15:00 UTC

Next update

14 May 15:00 UTC

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