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Churfirsten and Rhine Valley

Appenzeller Alpen

Sun 22 Mar

Stable day. Low, and the bulletin names no distinct problem — the ordinary care that steep terrain always needs.

Day Risk Profile

Low

Avalanche Problems

Dry avalanches · all day
Dry snow level 1 No distinct problem 1
N, NE, E, SE, SW, W, NW
above 1400m
Individual 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 extremely steep terrain. Mostly avalanches are small. Restraint should be exercised because avalanches can sweep people along and give rise to falls.
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.

Source: SLF Avalanche Bulletin Interpretation Guide

Snowpack & Weather

Snowpack

With the new fallen snow and southerly wind, snowdrift accumulations will form, some of which are prone to triggering. These are little more prevalent and larger along the Main Alpine Ridge. Elsewhere, they are mostly small.

In some places, Transparent, frequently flat crystals forming on the snowpack when moist air settles on the surface. It forms most often during cold, clear, humid nights. Once it is blanketed by fresh fallen snow, surface hoar is one of the most critical weak layer. See also: www.snowcrystals.itEAWS glossary that has been covered by snow is present in the uppermost section of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary, particularly on shady slopes. In this 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, avalanches have continued to be triggered in recent days, especially in southern Valais and in Grisons.

In the 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 near the ground, isolated avalanches have continued to be triggered recently, especially in the inneralpine regions and southern parts of Grisons. In the other regions, there are still weak layers in the near-ground Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary in some places on shady slopes, but they are mostly so thickly covered that they are hardly prone to triggering.

Weather review for Saturday

During the night it was partly cloudy in the east and south, and outgoing longwave radiation was somewhat reduced. During the day there were some bright spells in the west, in Valais and in Grisons, while elsewhere it was mostly cloudy.

Fresh snow

-

Temperature

At midday at 2000 m, between 0 °C in the west and -2 °C in the east and south

Wind

Mostly light from northerly directions

Weather forecast to Sunday

During the night a little snow will fall over a wide area. During the day, snow will continue to fall, primarily in the west and in the south. During the day it will be quite sunny in the east. In the Bernese Oberland, in Valais and in the Engadine there will be increasing bright spells. In the south and in the far west it will often remain cloudy.

Fresh snow

From Saturday afternoon to Sunday afternoon, the following amounts of snow will fall above approximately 1500 m:

  • Main Alpine Ridge in Upper Valais, directly on the border with Italy, western Ticino: 15 to 30 cm
  • Extreme west of Lower Valais and remaining Main Alpine Ridge and to the south of it: 5 to 15 cm
  • Elsewhere a widespread few centimetres

Temperature

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

Wind

Moderate southerly wind along the Main Alpine Ridge and along the northern Alpine ridgeline. A moderate foehn wind in some places in the northern Alpine valleys, elsewhere mostly light

Outlook to Tuesday

On Monday it will be mostly cloudy from the Bernese Oberland to eastern Switzerland. A small amount of snow will fall in showers above approximately 1200 m. Elsewhere there will be prolonged bright spells. Conditions will be sunny in the south. On Tuesday it will be sunny after a clear night. On Monday, there will be a moderate northerly wind at high altitudes. On Tuesday the wind will be mostly light. The zero-degree level will be just below 2000 m on Monday and at 2000 m on Tuesday.

The avalanche danger will not change significantly for Monday. Particularly in the south, snowdrift accumulations prone to triggering will form with a northerly wind in some places. On Tuesday the avalanche danger will decrease. Wet and gliding avalanches are still hardly to be expected.

Source

SLF

Issued

22 Mar 07:00 UTC

Valid until

22 Mar 16:00 UTC

Next update

22 Mar 16:00 UTC

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