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Avalanche Forecast

Archived

Feb 11th, 2023–Feb 12th, 2023

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Tumbler.

Warm temperatures on Sunday will make higher elevations a lot more enticing than lower down, potentially drawing you into places where winds have been hard at work forming new slabs. Make observations as you travel to avoid pockets of wind loaded snow and be especially wary of shallow rocky start zones in the alpine.

Confidence

Low

Avalanche Summary

No new avalanches have been reported, but field information is very limited in this region.

We suspect users who head to the backcountry will see evidence of a natural wind slab avalanche cycle from recent storm snow and strong southwest winds.

Snowpack Summary

20-40 cm of snow gradually accumulating over the past week is being redistributed by strong to extreme southwest winds into lee terrain in wind-exposed areas. particularly at upper elevations.

This recent snow overlies previous wind-affected snow as well as a melt-freeze crust found on sun-exposed slopes and on all aspects below 1600 m. The bond at this interface is reportedly quite strong in the adjacent west Rockies and Cariboos but remains worthy of investigation in this region where it lies more certainly within a human triggering depth.

Several more crust/facet/surface hoar layers exist in the upper and middle portions of the snowpack, however professionals in adjacent regions are beginning to de-emphasize them. The most concerning persistent weak layer by a mile is at the base of the snowpack, composed of large and weak facets formed in November. This layer is widespread and most likely triggerable in steep, rocky alpine terrain.

In general, the snowpack is weaker and shallower in this area than in areas farther west, with an average snowpack depth of around 100 cm at treeline. This makes deep persistent slab problems here quite a bit more concerning.

Weather Summary

Saturday night

Cloudy with isolated flurries. Strong southwest winds.

Sunday

Cloudy with flurries bringing 5-10 cm of new snow. Strong to extreme southwest winds. Treeline high temperatures around 0 with freezing levels rising to 1700 metres.

Monday

Mainly cloudy with isolated flurries. Moderate to strong southwest winds easing to light west over the day. Treeline high temperatures around -6.

Tuesday

Mainly sunny. Light north winds shifting southwest. Treeline high temperatures around -8.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be careful with wind slabs, especially in steep, unsupported and/or convex terrain features.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.
  • Avalanche hazard may have improved, but be mindful that deep instabilities are still present.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.