Wind Slabs
- Alpin
- Limite forestière
- Sous la limite forestière
- Probabilité
- Possible - Likely
- Taille
- 1–2
Recent snowfall and westerly winds are expected to have formed wind slabs in lee features in the alpine and treeline.
Avalanche danger will increase as temperatures rise throughout the day. There is uncertainty around how the snowpack will handle this warm-up.
Choose increasingly conservative terrain as temperatures rise.
Recent snowfall and westerly winds are expected to have formed wind slabs in lee features in the alpine and treeline.
Cornices have grown significantly in the past two weeks. Warm temperatures may make cause cornices to become weak. Cornice failures are dangerous on their own, but also have the potential to trigger larger avalanches on the slopes below.
Give them a wide berth when travelling on ridge-lines and minimize overhead exposure to large cornices.
This is mainly a concern in the western part of the region that received greater snowfall amounts last week. 30 to 70 cm of settled storm snow has shown evidence of forming a persistent slab above weak layers. The most reactivity has been observed on south-facing aspects, with reports of a poor bond to underlying sun crust layers. Weak surface hoar crystals may also exist in isolated areas on north-facing slopes.
MONDAY NIGHT: Cloudy with isolated flurries. Light westerly winds. Freezing level around 1000 m.
TUESDAY: Partially cloudy. Light to moderate westerly winds. Freezing level rising to 2000 m.
WEDNESDAY: Mainly cloudy, light flurries. Moderate to strong westerly winds. Freezing level around 2000 m.
THURSDAY: Mainly clear. Light northwesterly winds. Freezing level around 1000 m.
Several natural and one human-triggered wind slabs occurred in the northwest of the region on Sunday in the alpine and treeline (size 1-2.5).
We have heightened concern about a developing persistent slab problem in some parts of the Purcells (read more in this blog).
Several notable human-triggered slab avalanches occurred last week, suggesting that the recent snow is bonding poorly to the underlying layers. These occurred on a range of aspects above 2000 m, with the most notable reactivity observed on south-facing aspects. Most slabs were small in the top 20 to 30 cm of snow (size 1), but one larger 70 cm thick slab was remotely triggered from below by a group of skiers (size 2). This avalanche occurred on a south aspect at 2250 m.
10-20 cm of recent snowfall overlies last week's 30-70 cm of settled storm snow. Snow depths taper significantly with elevation, with moist and crusty surfaces below 1800 m and on south aspects into the alpine.
In some areas, last week's snow is well bonded to old crust layers, while in other areas the snow has settled into a reactive slab above weak layers around the crusts. At this point, it appears persistent slab problems could be developing in the deeper snowpack areas along the western side of the range. The lower snowpack is generally well bonded.