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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

Cariboos, Blue River, Clearwater, McBride, Premier, Quesnel, Sugarbowl, Clemina, North Monashee, Renshaw, Robson.

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. Then stick to it! Surface slides entraining recent accumulations or stepping down to a deeper weak layer could result in surprisingly large and destructive avalanches on Thursday.

Confidence

Moderate

Avalanche Summary

Improving observations from operators in the region observing up to 25% of their tenures since the weekend storm generally show no new avalanches. Reports closer to the immediate aftermath of the storm described numerous small dry loose avalanches and several storm slabs releasing with skier traffic and ski cutting, generally below treeline and limited to size 1 or smaller.

We expect some degree of a natural avalanche cycle also took place during the storm at higher, wind affected elevations, especially in areas that were on the higher end of our new snow totals. This MIN report from Westridge gives a good indication of conditions that were likely fairly widespread in the region.

A few very large (size 3.5 to 4) deep persistent slab avalanches were also observed over last week, which likely occurred during the very windy arctic outflow event.

Looking forward, moderate snowfall and high winds are expected to trigger an uptick in natural avalanche activity and human triggering potential through Thursday.

Snowpack Summary

10-20 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 50 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.

A small layer of surface hoar crystals may be found about 70 to 130 cm deep, particularly in areas sheltered from the wind around treeline. This layer had been gaining strength prior to the last storm and is currently considered dormant. We are still light on observations showing whether it did or didn't wake up in isolated areas from the weight of the recent snow.

Large and weak facets that formed in November are found near the base of the snowpack. Although the likelihood of triggering this layer is low at this time, the consequence of doing so remains very high. This layer is most likely to be human-triggered in thin, rocky slopes at alpine and upper treeline elevations.

Weather Summary

Wednesday night

Cloudy with increasing flurries bringing 5-10 cm of new snow. Strong to extreme southwest winds.

Thursday

Cloudy with continuing snowfall bringing another 5-15 cm of new snow. Strong southwest winds easing over the day. Treeline high temperatures around -8.

Friday

Cloudy with easing flurries bringing up to 5 cm of new snow and storm totals to 20-30 cm. Light southwest winds. Treeline high temperatures around -9.

Saturday

A mix of sun and cloud. Light east winds. Treeline high temperatures around -8.

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.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.

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.