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Avalanche Forecast

Archived

Mar 1st, 2023–Mar 2nd, 2023

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

Regions

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

Make a plan to step back from avalanche terrain and away from overhead hazard as the storm progresses and avalanche danger increases over the day. Surface slides entraining recent accumulations or stepping down to a deeper weak layer could result in surprisingly large and destructive avalanches.

The possibility for very large deep persistent slab avalanches should not be ruled out.

Confidence

Moderate

Avalanche Summary

We have preliminary reports of a serious avalanche incident today near Invermere, which is directly adjacent to this forecast region. We will update this section with details as they become available.

Almost all operators in the region reported some variation of the theme of a natural and skier-triggered avalanche cycle early this week as 40-70 cm of new snow weekend settled into touchy storm slabs in some areas and produced powerful dry loose releases with rider traffic in areas where slabs hadn't quite formed. Improved travel conditions on Monday and Tuesday allowed for more observations of the aftermath of the cycle, generally observed to have produced avalanches to size 2.5 (large!) and for the most part confined to the depth of new snow. A few operators noted the cycle being less widespread than expected.

Clear skies last week 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. Another one was triggered in Glacier National Park on Monday. These avalanches have been occurring on all aspects and generally between 2200 m and 2800 m in elevation. Although many of these avalanches have 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.

Looking forward, moderate snowfall and elevated winds are expected to trigger an uptick in natural avalanche activity and human triggering potential through Thursday. The possibility for very large deep persistent slab avalanches should not be ruled out.

Snowpack Summary

15-25 cm of new snow is expected to accumulate in the region by end of day Thursday. For the most part it will add to low density storm snow from the weekend, but it may also bury recent wind slabs in more exposed areas and likely a thin sun crust on sun-exposed aspects.

The roughly 40-80 cm of new snow from the weekend storm sits on an interface that includes small surface hoar in lower elevation sheltered areas and more widespread faceted (sugary) snow and heavy wind effect. This interface remains in question with storm slabs having been generally slow to form over it in recent days.

Around 100 to 130 cm of snow may now 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, alarming reports like this one from Glacier National Park continue to trickle in, confirming it is still best to avoid steep, thin, rocky slopes near ridges at alpine and upper treeline elevations.

Weather Summary

Wednesday night

Cloudy with flurries bringing about 5 cm of new snow. Light southwest winds increasing into the morning.

Thursday

Cloudy with continuing snowfall bringing 10-20 cm of new snow. Moderate southwest winds, strong in the alpine. Treeline high temperatures around -7.

Friday

Cloudy with continuing flurries bringing about 5 cm of new snow and storm totals to 20-30 cm. Light to moderate southwest winds. Treeline high temperatures around -8.

Saturday

Mainly cloudy with isolated flurries. Light southeast winds. Treeline high temperatures around -7.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.
  • 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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.

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.