Showing Thu 19 Feb 2026 Back to today

Churfirsten and Rhine Valley

Appenzeller Alpen

Thu 19 Feb

Day Risk Profile

Considerable · lower end of the band

Avalanche Problems

Dry avalanches · all day
Dry snow level 3 Wind slab 3-
N, NE, E, SE, W, NW
above 1600m
Fresh and somewhat older wind slabs are in some cases prone to triggering. They can be released even by a single winter sport participant. The 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 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. Backcountry touring calls for experience in the assessment of avalanche danger.
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

Snowpack & Weather

Snowpack

In the west and north, many large and very large naturally triggered avalanches have occurred in recent days. There have also been some isolated extremely large avalanches in Valais. Natural avalanche activity decreased significantly on Wednesday. In the regions exposed to heavier precipitation in the west and north, this week's thick layers of new and drifted snow are gradually settling and consolidating. Naturally triggered very large avalanches are now possible only in isolated case. Fresh snow and westerly winds will result in widespread fresh snowdrift accumulations on Thursday.

This week's layers of fresh and drifted snow are thinner in Ticino, Grisons and some regions in southern Valais than they are further north and are lying on an unstable Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary with 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. Human activity can still very easily trigger avalanches, even over relatively large distances, in the old snowpack.

Weather review for Wednesday

After a break in the precipitation overnight to Wednesday, light precipitation set in in the west and north. The snowfall level was between 1000 and 1500 m. There were sunny intervals in the south and southeast.

Fresh snow

From Tuesday afternoon to Wednesday afternoon above approximately 1800 m:

  • Lower Valais, northern Valais, northern flank of the Alps, Jura, northern Grisons, Lower Engadine a widespread 5 to 15 cm; central and eastern flank of the Alps up to 30 cm
  • elsewhere a few centimetres; dry in the far south

Temperature

At midday at 2000 m, around -2 °C in the west and south, around -5 °C in the east

Wind

  • In the north, moderate to strong northwesterly during the night and westerly to southwesterly during the day
  • In the south, light to moderate northerly, backing southwesterly.
Weather forecast to Thursday

There will mainly be heavy cloud cover with widespread precipitation, centred in the far west and in the Upper Engadine. The snowfall level will be around 1000 m in the north and around 700 m in the south.

Fresh snow

From Wednesday evening to Thursday afternoon above approximately 1600 m:

  • extreme west of Lower Valais, Vaud and Fribourg Alps, Moesano, Avers, Val Bregaglia, Corvatsch, Bernina region, Val Poschiavo: 20 to 30 cm
  • elsewhere a widespread approximately 10 cm with up to 20 cm in eastern Ticino and Grisons

Temperature

At midday at 2000 m, around -3 °C

Wind

  • Overnight to Thursday, moderate to strong southwesterly, temporarily foehn-like in the Alpine valleys
  • Veering westerly to northwesterly over the course of the day, moderate to strong at high altitudes
Outlook to Saturday

On Friday, conditions will be cloudy in the north and 15 to 30 cm of snow will fall. The snowfall level will be between 600 and 900 m. The precipitation forecast is still uncertain. In the south, conditions will be sunny with a northerly wind and brighter in the inneralpine regions. There will be sunny conditions in Valais and the south on Saturday Elsewhere there will be broken cloud and a little precipitation will be possible. The snowfall level will rise to 1500 m. On both days, there will be a northwesterly wind, moderate to strong and occasionally storm-force at high altitudes.

Avalanche danger will decrease and hardly any very large naturally triggered avalanches are to be expected. In western and northern regions with a lot of snow, human activity may trigger avalanches, especially in the near-surface layers of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary. In some regions in southern Valais, northern Ticino and Grisons, avalanche danger will decrease only very slowly due to the thin snow cover on the very weak Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. In these regions, conditions for touring and off-piste skiing remain critical in many places.

Source

SLF

Issued

19 Feb 07:00 UTC

Valid until

19 Feb 16:00 UTC

Next update

19 Feb 16:00 UTC

See this region on the map