Churfirsten and Rhine Valley
Appenzeller Alpen
Avalanche Problems
No distinct problem
1
Field notes
SLF uses this label when no single problem dominates the assessment, often on lower-danger days. It doesn't mean conditions are safe: any avalanche type is still possible, and normal caution applies. On stable days this is usually a signal to enjoy the mountains with general awareness; on less-stable days where the assessment is still inconclusive, it's a signal to be cautious specifically because there's no clear pattern to follow.
Gliding snow
1
Field notes
Almost impossible to predict precisely, even when the warning signs are visible. A crack visible on the snowpack surface formed by snow-gliding on steep, and particularly grass-covered slopes. Areas below slopes with visible glide cracks should be avoided whenever possible due to threat of gliding sluffs or avalanches.EAWS glossary — gaps that open in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary down to the ground — are often precursors to release, but they don't tell you when. A glide avalanche can release minutes after the cracks appear, or weeks later, or not at all. Some release without any visible warning. Avoid lingering anywhere near glide cracks: above them, alongside them, or below in the runout.
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.