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Prättigau and Davos

Nördliches Prättigau

Tue 16 Dec

Avalanche Problems

Low (1) Dry avalanches · all day
Dry snow level 1 Persistent weak layers 1
All aspects
above 2000m
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 the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary can still be released in very isolated cases in particular on extremely steep shady slopes. In addition clearly visible wind slabs will form especially 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. These are small but can in some cases be released easily. They are to be evaluated with care and prudence in very steep terrain. In Areas above approximately 3000 m (particularly glaciated areas).EAWS glossary and in the regions exposed to the foehn wind these Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are more prevalent and the danger is slightly greater. Mostly avalanches are small. Apart from the danger of being buried, restraint should be exercised in particular in view of the danger of avalanches sweeping people along and giving rise to falls.
Field notes

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

The snow depths at intermediate and high altitudes are generally below average for the time of year. There is particularly little snow on the southern flank of the Alps. Only in parts of Lower Valais is snow depth roughly in line with the long-term average. On southern slopes and generally below 2400 m, the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is mostly crusted.

Along the Main Alpine Ridge and south of there, fresh and drifted snow will be deposited at high altitudes on a thin but heavily faceted Snow deposited on the ground in a multiplicity of layers.EAWS glossary on Tuesday. Avalanches are particularly likely to be triggered in these regions.

North of the Main Alpine Ridge, there are 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 in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary, particularly on northern and eastern slopes above approximately 2400 m, but hardly any avalanches have been triggered there in recent days by human activity. At high altitudes the strong southerly wind may transport some of the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary, resulting in snowdrift accumulations locally prone to triggering.

Weather review for Monday

Conditions were mostly sunny in the mountains, with high broken cloud gathering in the south-west and south from midday.

Fresh snow

-

Temperature

At midday at 2000 m, between +4°C in the north and +1°C in the south

Wind

In the Alpine valleys in the north and generally at high altitudes, moderate, at times strong from southerly directions

Weather forecast to Tuesday

Towards Tuesday morning, precipitation will set in on the Main Alpine Ridge and south of there. The snowfall level will be at around 1200 m. In other regions, it will be mostly cloudy but dry.

Fresh snow

The following amounts will fall above 1600 m by Tuesday afternoon:

  • Main Alpine Ridge from the Grand St Bernard Pass to the Bernina and south of there: 5 to 15 cm, with up to 20 cm in western Ticino and the Simplon region
  • elsewhere dry

Temperature

At midday at 2000 m, between +4°C in the north and -2°C in the south

Wind

In the Alpine valleys in the north and generally at high altitudes, at times strong from southerly directions

Outlook to Thursday

During the night to Wednesday and on Wednesday morning it will be cloudy on the southern flanks of the Alps and in Grisons. Some snow may fall above 1600 m. In other regions, Wednesday will be very sunny. On Thursday conditions will be very cloudy but dry on the southern flank of the Alps, with sunny conditions elsewhere. Winds will be mostly light on Wednesday, and occasionally moderate on Thursday, from the southwest.

Avalanche risk may continue to increase slightly during the night to Wednesday on the southern flank of the Alps, but elsewhere will barely change.

Source

SLF

Issued

16 Dec 06:17 UTC

Valid until

16 Dec 16:00 UTC

Next update

16 Dec 16:00 UTC

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