Gliding snow
- All elevations
- Size
- 2
Stability: very poor · Frequency: some
Gliding snow represents the main danger. Wind slabs require caution.
Stability: very poor · Frequency: some
Stability: poor · Frequency: some
Gliding snow represents the main danger. Wind slabs require caution.
As a consequence of warming more medium-sized gliding avalanches are possible. This applies on steep grassy slopes. The no longer entirely fresh wind slabs are in some cases prone to triggering on steep shady slopes. Caution is to be exercised in particular above approximately 2200 m, as well as in gullies and bowls, and behind abrupt changes in the terrain.
The fresh and somewhat older wind slabs are lying on soft layers in particular on near-ridge shady slopes at elevated altitudes. As a consequence of rising temperatures the snow drift accumulations will stabilise. The old snowpack is wet, in particular at low and intermediate altitudes.
Gradual increase in danger of gliding avalanches as a consequence of warming.
Bulletin data: Avalanche Warning Service Tirol, avalanche.report (CC BY 4.0)