Wind Slabs
- Alta quota
- Limite del bosco
- Sotto il limite del bosco
- Probabilità
- Possible - Likely
- Dimensione
- 1–2
Increasing southwest winds are expected to move Tuesday's snow into new wind slabs on leeward slopes, particularly near ridgetop.
Limited observations are keeping forecast confidence low. Recent snow is expected to remain reactive to triggering on Thursday.
Increasing southwest winds are expected to move Tuesday's snow into new wind slabs on leeward slopes, particularly near ridgetop.
New snow accumulations exposed to strong sunshine will be increasingly likely to shed from steep slopes on Thursday. This may occur naturally or with a human trigger.
Weak snow at the bottom of the snowpack hasn't gone away. Evidence of deep persistent slab avalanches has been focused in the Sparwood-Elkford area over the past month. Human triggering is most likely around steep, rocky terrain features or anywhere the snowpack is thin and weak. A failing cornice could initiate a deep persistent slab when it impacts the slope below.
Wednesday night: Becoming clear. Light northwest winds.
Thursday: Sunny with cloud developing in the afternoon. Light to moderate west winds. Alpine high temperatures around -5.
Friday: Mainly cloudy. Light to moderate west or southwest winds. Alpine high temperatures around -5
Saturday: Mainly cloudy. Light to moderate southwest winds. Alpine high temperatures around -4.
No new avalanches were reported from Tuesday's storm, but observations have been minimal. The new snow is expected to remain reactive over the near term, especially on steeper south facing slopes and in areas where wind loading has occurred or will occur.
About 15-25 cm of new snow accumulated during Tuesday's storm. The new snow likely sits above a melt-freeze crust on sun-exposed slopes and on previously wind-affected snow in other areas, so new slabs may take some time to bond to these surfaces.
A layer of faceted grains overly a melt-freeze crust from early February. This layer currently sits 40 to 80 cm below the surface.
The base of the snowpack contains basal facets that are most prominent in shallow, rocky start zones.