Showing Thu 9 Apr 2026 Back to today

Schober Group West

Schobergruppe West

Thu 9 Apr

Day Risk Profile

Low
Earlier
Moderate
below 2400m
Later
Low
above 2400m
Later

Avalanche Problems

Below 2400 m

Moderate (2) Wet avalanches, later
Wet snow level 2 Wet snow Slab 2
All aspects
below 2400m
Medium Few Poor
GM.10 GM.1
Field notes

Rolling snowballs, deep penetration when you step or ski, and small natural slides are clear signals that the Snow deposited on the ground in a multiplicity of layers.EAWS glossary is losing strength. After a clear, cold night the surface often freezes into a strong supporting Layer of hard-compacted snow resulting from a melt-freeze process or wind.EAWS glossary, and conditions are favourable in the early morning. After a warm, overcast night, the problem may be present from the start of the day. Plan early returns and watch the runout zones below you.

Source: SLF Avalanche Bulletin Interpretation Guide

Above 2400 m

Low (1) Dry avalanches, earlier
Dry snow level 1 Persistent weak layers Slab 1
N, NE, E, W, NW
above 2400m
Medium Poor
GM.10 GM.1
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

Low (1) Dry avalanches, later
Dry snow level 1 Persistent weak layers Slab 1
N, NE, E, W, NW
above 2400m
Medium Poor
GM.10 GM.1
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

Avalanche Activity

Increase in avalanche danger as a consequence of warming during the day and solar radiation. Weak layers in the old snowpack can still be released in very isolated cases.

The avalanche conditions in the morning are mostly favourable. As a consequence of warming during the day and the solar radiation, the likelihood of wet avalanches being released will increase. This applies in all Direction in which a slope faces as indicated by compass direction of the fall line; i.e. a north slope faces in a northerly direction.EAWS glossary below approximately 2400 m, and on south facing slopes at elevated altitudes. Sometimes avalanches are medium-sized and can be released also by a single winter sport participant. In very isolated cases dry avalanches can also be released in the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. 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 on very steep west, north and east facing slopes above approximately 2400 m. Avalanches can reach medium size. Restraint should be exercised because avalanches can sweep people along and give rise to falls.

Outlook

Constant avalanche danger

10 April 2026

Hardly any decrease in danger of moist and wet avalanches as the temperature drops.

Snowpack & Weather

Snowpack
Outgoing longwave radiation during the night will be good. The surface of the Snow deposited on the ground in a multiplicity of layers.EAWS glossary will freeze to form a strong Layer of hard-compacted snow resulting from a melt-freeze process or wind.EAWS glossary and will already soften in the late morning. Sunshine and high temperatures will give rise to increasing and thorough wetting of the snowpack. The old wind slabs are lying on top of a weakly bonded Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary in particular on west, north and east facing slopes above approximately 2400 m.

Source

ALBINA

Issued

8 Apr 15:00 UTC

Valid until

9 Apr 15:00 UTC

Next update

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