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Avalanche Forecast

Archived

Feb 26th, 2023–Feb 27th, 2023

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

Regions

North Columbia, South Columbia, Esplanade, Jordan, North Selkirk, Shuswap, West Purcell, Badshot-Battle, Central Selkirk, Goat, Gold, Kokanee, North Okanagan, Retallack, Valhalla, Whatshan.

Don't be too quick to rule out the storm slab problem. That heap of new snow sits on a questionable interface and more is on tap for Sunday night. Use low consequence slopes to assess the new snow's bond and raise your guard as you approach exposed terrain where new wind slabs present a more certain hazard.

Confidence

Moderate

Avalanche Summary

Observations of new avalanche activity from Saturday and Sunday are still limited to reports from the early hours of the storm when a small storm slab problem began to take shape. We anticipate some degree of a natural avalanche cycle has since place throughout the region but especially where 30 cm or more new snow accumulated.

On Friday, we received reports of many natural, explosive, and human-triggered storm slab and wind slab avalanches from all aspects. The majority of this activity occurred at treeline and in the alpine, and was typically around size 2 with a few up to size 3. The typical release depth of these avalanches varied from 20 to 60 cm.

Clear skies a few days ago allowed for observations of many deep persistent slab avalanches as well as explosive control missions, which produced large to very large (size 2 to 3.5) avalanches. They were on all aspects and between 2200 m and 2800 m in elevation. Although many of the avalanches occurred in unrideable terrain, they are evidence that the weak basal snowpack is still triggerable. Riders should continue to avoid thin snowpack areas, which are often found near ridgelines.

Snowpack Summary

Stormy conditions brought up to about 40 cm of new snow to the region along with strong southwest wind on Saturday. The new snow buried an interface from the recent cold period which includes faceted (sugary) surface snow, small surface hoar in sheltered areas, and widespread heavy wind effect and wind slabs in exposed terrain from recent northeast winds. Below this interface is 20-50 cm of older storm snow from the beginning of last week.

Around 80 to 100 cm of snow may rest on a small layer of surface hoar crystals that was buried mid-February. This layer is most likely found around treeline elevations in areas sheltered from the wind. This layer generally appears to be dormant now but could still be capable of producing avalanches in isolated areas. The remainder of the mid-snowpack is generally strong.

A layer of large and weak facets that formed in November is deeply buried, found near the base of the snowpack. The likelihood of human triggering this layer is currently low given its depth. However, it is still best to avoid steep, thin, rocky slopes near ridges at alpine and upper treeline elevations.

Weather Summary

Sunday night

A final round of convective flurries bringing up to about 5 cm of new snow. Light to moderate southwest winds easing into the morning.

Monday

Mainly cloudy with isolated flurries. Light south winds. Treeline high temperatures around -9 °C.

Tuesday

Mainly cloudy with isolated flurries. Light east or southeast winds. Treeline high temperatures around -8 °C.

Wednesday

Mainly cloudy with isolated flurries. Light west winds. Treeline high temperatures around -8.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid all avalanche terrain during periods of heavy snowfall.
  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Approach steep open slopes at and below treeline cautiously, buried surface hoar may exist.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.