Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 28th, 2023–Mar 1st, 2023

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

Regions

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

There's a ton of snow available for forecast winds to build new slabs with on Wednesday. Be ready to back off from features that have signs of previous or especially active wind loading. The potential for dry loose avalanches on steep slopes will also need to be managed as you duck into sheltered terrain.

Confidence

Moderate

Avalanche Summary

Limited observations from operators in the region observing 5-15% of their tenures after the weekend storm detail 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 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, the next storm hits the region late Wednesday, but with elevated winds leading the charge and expected to be the initial driver of avalanche hazard during the day.

Snowpack Summary

Steep south aspects may now have a thin sun crust from clearing skies on Monday and Tuesday. The upper snowpack is otherwise composed of up to about 50 cm of new snow from stormy conditions over the weekend. The new snow buried an interface which includes faceted (sugary) surface snow, small surface hoar in lower elevation sheltered areas, and more widespread heavy wind effect and wind slabs at higher elevations from previous northeast winds.

Prior to the storm, a small layer of surface hoar crystals could be found about 50 to 100 cm deep, particularly in areas sheltered from the wind around treeline. This layer appears to be gaining strength and is currently considered dormant, but we're still light on observations showing whether it did or didn't wake up in isolated areas from the weight of the new 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

Tuesday night

Partly cloudy. Light west winds becoming moderate southwest.

Wednesday

Cloudy with isolated flurries, increasing in late afternoon and overnight. Winds approaching strong southwest by end of day. Treeline high temperatures around -10.

Thursday

Cloudy with continuing snowfall bringing 10-15 cm of new snow, including overnight amounts. Strong southwest winds easing over the day. Treeline high temperatures around -8.

Friday

Cloudy with continuing snowfall bringing 5-15 cm of new snow, including overnight amounts. Moderate southwest winds. Treeline high temperatures around -9.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Pay attention to the wind, once it starts to blow fresh sensitive wind slabs are likely to form.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Wind slabs are most reactive during their formation.
  • Be aware of the potential for loose avalanches in steep terrain where snow hasn't formed a slab.

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 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.