Avalanche danger • Weißkugelgruppe region • 2025/26
Link copied
Weißkugel Group
Weißkugelgruppe
Wed 18 Feb
Updated off-schedule
The provider reissued this bulletin at 18 Feb 09:27 UTC, outside the normal publication cycle.
Day Risk Profile
2
Moderate
below 2100m
4
High
above 2100m
Avalanche Problems
Above 2100 m
High
(4)
Dry avalanches
· all day
Persistent weak layersSlab4
N, NE, E, W, NW
above 2100m
LargeManyVery poor
GM.1GM.6
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.
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.
Weak layers in the old snowpack can be released very easily. Fresh wind slabs are to be evaluated critically.
Distinct 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 be released very easily. This applies on west, north and east facing slopes above approximately 2100 m. Avalanches can 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 prevalent and are difficult 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 the formation of shooting cracks when stepping on the Snow deposited on the ground in a multiplicity of layers.EAWS glossary and fresh avalanches serve as an alarm indicating the danger. Remotely triggered avalanches are possible. In addition the fresh wind slabs of the last few days 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 are prone to triggering in some locations. Such avalanche prone locations are to be found 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 above the tree line. Individual avalanche prone locations are to be found also in areas close to the tree line. The prevalence of avalanche prone locations and likelihood of triggering will increase with altitude. The avalanche situation is a little more favourable in highly frequented terrain.
Outlook
→Constant avalanche danger
19 February 2026
Weak layers in the old snowpack represent the main danger. <br/> <br/> Thursday: <br/> As a consequence of new snow and wind a dangerous avalanche situation will persist.
Snowpack & Weather
Snowpack▾
Over a wide area 20 to 40 cm of snow, and even more in some localities, has fallen since Sunday. The wind was strong to storm force at times. The Snow deposited on the ground in a multiplicity of layers.EAWS glossary will be prone to triggering. The new snow and wind slabs are bonding only slowly with the Snow layers deposited from earlier precipitation, prior to fresh fallen snow. Old snow layers consist of metamorphosed snow crystals.EAWS glossary. In some places various wind slab layers are lying on 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. Distinct 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 exist in the bottom section of the snowpack on west, north and east facing slopes. Reports filed by observers and released avalanches confirm the distinct avalanche danger.
Snowdesk needs a refreshIt couldn't update itself. Reload to finish.ReloadDismissUpdating…Updating SnowdeskApplying the new version — the page will reload in a moment.
Update required
This version of Snowdesk is no longer supported. Reload to continue.
Install Snowdesk
Add Snowdesk to your home screen for one-tap access and a full-screen map. Downloaded areas read without a signal either way.
Add Snowdesk to your Home Screen
Tap the Share icon, then choose Add to Home Screen. Snowdesk then opens full screen. Downloaded areas read without a signal either way.
Reset local data
Snowdesk needs to reset local data on this device to keep working. Your
account and everything saved to it are stored on the server and are not affected.
Some changes couldn't be saved and won't be retried.
Snowdesk has not been saved on this device yet, so switching Offline mode on will stop it
opening at all until you switch it off again.
Switch it on anyway?Custom area %(n)sGetting ready…Getting ready… (%(n)s of %(total)s)Ready — %(total)s areas up to dateReady — 1 area up to date%(ready)s of %(total)s ready%(n)s changes still waiting to send1 change still waiting to sendBulletins from %(day)s%(metres)s m altitudeNo bulletin coverage for this location.Rating expired — reconnect to see today's danger levelas of %(time)sShowing cached data — as of %(time)s