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Lower Valais

Val d'Anniviers

Wed 7 Jan

Avalanche Problems

Moderate (2-), lower end of the band Dry avalanches · all day
Dry snow level 2 Wind slab + Persistent weak layers 2-
All aspects
above 2400m
The fresh and older wind slabs are in some cases still prone to triggering. They are mostly small. They are to be evaluated with care and prudence in very steep terrain. Avalanches can additionally in very isolated cases be released in the weakly bonded old snow also. Avalanches can in some cases reach medium size. Careful route selection is recommended.
Field notes

Wind slab

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.

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

On the northern flank of the Alps, the fresh and drifted snow which has fallen over the last week on high-altitude wind-protected shady slopes is lying on an often faceted and therefore weak old snow surface. Elsewhere, the snow surface has often been shaped by the wind and is frequently frozen solid below 2400 m.

In western and northern Lower Valais, the Snow deposited on the ground in a multiplicity of layers.EAWS glossary structure is relatively favourable.

In other regions, the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is thin and weak, and mostly consists of Snow grains, solid, with multiple flat glassy faces and sharp edges. Developed from faceting metamorphism, usually poorly bonded to one another (fewer contact points), a critical factor in avalanches if a faceted layer is covered with bonded snow. Typical grain size: 0.5 to 3 mm See also: www.snowcrystals.itEAWS glossary with embedded crusts. Snowdrift accumulations deposited on top of this snowpack are in some cases triggerable. In addition, isolated avalanches in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary close to the ground cannot be ruled out, especially on the Main Alpine Ridge in Upper Valais and on the central part of the southern flank of the Alps. However, no more such avalanches have been reported in the last week.

Weather review for Tuesday

It was sunny and cold in the mountains.

Fresh snow

-

Temperature

At midday at 2000 m, around -12 °C in the north and -8 °C in the south

Wind

Northerly wind:

  • Moderate to strong along the Main Alpine Ridge and to the south of it
  • Elsewhere mostly light
Weather forecast to Wednesday

In the mountains it will be sunny and remain cold.

Fresh snow

-

Temperature

At midday at 2000 m, around -12 °C

Wind

Northwesterly wind:

  • Moderate on the Main Alpine Ridge and to the south of it, sometimes strong in the afternoon at higher altitudes
  • Elsewhere light to moderate
Outlook to Friday

There will be widespread precipitation on Thursday and Friday, which will be intense in the west and north from Thursday afternoon. In the extreme west of Lower Valais and northern Lower Valais, a total of 60 to 80 cm of snow is expected to fall; in the rest of Valais and on the northern flank of the Alps, 30 to 60 cm is expected. The snowfall level will increase temporarily to 1600 m in the west and north overnight to Friday, and will remain at low altitude elsewhere. The snowfall will be accompanied by a strong to storm-force westerly wind.

The avalanche danger will increase significantly in the west and north. Danger level 4, high, is expected to be reached in Lower Valais on Friday. The avalanche danger will also increase slightly in Grisons, but will not change significantly in the south.

Source

SLF

Issued

6 Jan 14:51 UTC

Valid until

7 Jan 16:00 UTC

Next update

7 Jan 16:00 UTC

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