Gliding snow
- All elevations
- Size
- 2
Stability: very poor · Frequency: some
Gliding snow represents the main danger.
Stability: very poor · Frequency: some
The old snowpack is wet, in particular at low and intermediate altitudes. As a consequence of rising temperatures the snow drift accumulations stabilised.
As a consequence of the occasionally strong northwesterly wind, fresh snow drift accumulations will form.
Gliding snow represents the main danger.
As a consequence of warming more medium-sized gliding avalanches are possible. This applies on steep grassy slopes. The older wind slabs are in individual cases still prone to triggering on steep shady slopes. Very isolated avalanche prone locations are to be found in particular on very steep shady slopes at high altitude.
Bulletin data: Avalanche Warning Service Tirol, avalanche.report (CC BY 4.0)