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Prättigau and Davos

Südliches Prättigau

Thu 2 Apr

Hard-to-read day. Considerable, with persistent weak layers buried — no warning underfoot, so terrain choice is the only control left.

Day Risk Profile

Considerable

Avalanche Problems

Dry avalanches · all day
Dry snow level 3 Persistent weak layers 3=
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 represent the main danger. Avalanches can be released by a single winter sport participant and reach large size in isolated cases. The Locations delineated by aspect or altitude where avalanches can trigger and people or objects are at risk.EAWS glossary are barely recognisable, even to the trained eye. Caution is to be exercised on little-used, rather lightly snow-covered shady slopes. Backcountry touring calls for experience in the assessment of avalanche danger.
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

In the north, Tuesday's large volumes of fresh and drifted snow are gradually stabilizing. In some places, however, the fresh snow from recent days is lying on 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 and in some cases also buried 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, particularly on shady slopes. In these weak layers, avalanches can be triggered, which may occasionally become large.

In the inneralpine regions of Valais and especially Grisons, 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 deeper in the Snow deposited on the ground in a multiplicity of layers.EAWS glossary are also still prone to triggering in some places. Isolated avalanches may also be triggered in near-ground weak layers.

Weather review for Wednesday

Conditions were quite sunny in the west and south after a mostly clear night, while the east saw some sunny intervals.

Fresh snow

-

Temperature

At midday at 2000 m, between -8 °C in the north and -4 °C in the south

Wind

Northeasterly

  • strong at night, increasing to storm-force at times
  • easing to mostly moderate during the day
Weather forecast to Thursday

After a generally clear night, conditions will be quite sunny in the west and south, while the east will see some sunny intervals. Cloud will build up further in the afternoon, but it will remain mostly dry.

Fresh snow

-

Temperature

At midday at 2000 m, around -4 °C in the north and 0 °C in the south

Wind

  • Easing overnight to mainly light to moderate northeasterly
  • Increasingly moderate northerly during the day, strong in the afternoon on the main Alpine ridge
Outlook to Saturday

In the west and south, the nights will be mostly clear, and conditions will be mostly sunny during the daytime. In the east the nights will be partly cloudy and a few snowflakes may fall locally. Friday will be mostly sunny during the day, and Saturday daytime will see some bright periods. On Friday the wind will continue to be a moderate northerly at times, easing to mostly light on Saturday. The zero degree level will be at 1600 m on Friday in the north and at 2200 m in the south. On Saturday it will rise markedly, to 2800 m in the west and south and to 2400 m in the east.

The danger of dry avalanches will decrease. The danger of wet and gliding avalanches will increase over the course of each day. On Friday, this increase will remain slight but it will be more marked on Saturday. Ski touring should be started early and finished in good time.

Source

SLF

Issued

2 Apr 06:00 UTC

Valid until

2 Apr 15:00 UTC

Next update

2 Apr 15:00 UTC

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