Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Very Likely
- Dimensione
- 1.5–2.5
This wind slab is sitting on the Feb. 24 interface down 20-30cm and consists of facets and previous wind slab.
Approach all avalanche terrain with extreme caution. We are nearing a natural avalanche cycle.
This wind slab is sitting on the Feb. 24 interface down 20-30cm and consists of facets and previous wind slab.
This is the Feb 3 rain crust interface which has facets on top of the crust and can be found 40-50cm down.
This is the November basal facet problem that exists mostly in the high alpine above 2400m where the February 3 rain crusts disappears.
No avalanche activity was observed during the field day. This was surprising, given the amount of snow and wind. Maybe it is just waiting for a light trigger like a skier.
20-30cm of snow has fallen in this last storm and has become a wind slab in all exposed areas. This new wind slab and storm snow sits on top of a variety of layers:
The February 24 storm interface which is down about 20-30cm and consists of suncrust, previous wind slab. This layer will be sensitive to skier triggering.
The February 3 Rain crust which is down about 40-50cm. This crust has started to develop facets on top of it which is a perfect layer for sliding.
We are at or nearing the critical load of new snow or slab development for a natural avalanche cycle to start.
Tuesday will be a mixed bag of cloud, sun and isolated flurries. Expect cold temperatures in the morning of -26c in the alpine and then warming to -15c. Winds are forecast to be 25-30km/hr from the SW
Wednesday to Friday: Periods of snow with up to 45cm by Friday. Stay tuned for snow amounts and how it will impact the avalanche hazard...
More details can be found in the Mountain Weather Forecast.