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Avalanche Forecast

Archived

Mar 13th, 2021–Mar 14th, 2021

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.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Cariboos.

 Overhead hazards such as cornice failures and wet loose avalanches on large alpine slopes will be the primary concern on Sunday. Pay attention to what's above your head and back off of slopes if the snow surface becomes moist. 

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

  

SATURDAY NIGHT: Clear / Strong, southwest ridgetop wind / alpine low temperature -4 / Freezing level 1800 m.

SUNDAY: Sunny with increasing cloud in afternoon / Moderate, southwest ridgetop wind / alpine high temperature 0 / Freezing level 1800 m.

MONDAY: Sunny / Light, west ridgetop wind / alpine high temperature -2 / Freezing level 1400 m.

TUESDAY: Sunny / Light, west ridgetop wind / alpine high temperature -1 / Freezing level 1600 m.

Avalanche Summary

No avalanches were reported in this region on Friday. However, the rapidly rising freezing level and sunny skies are expected to elevate the avalanche hazard through the weekend.

Snowpack Summary

5-15 cm. of recent convective snow and moderate southwesterly winds have formed fresh wind slabs below alpine ridgetops. Dry snow can be found on north aspects and crusty snow surfaces exist on solar aspects. Large cornices loom over alpine ridgetops.

A persistent weak layer made up of surface hoar at treeline elevations and a crust with facets in the alpine on solar aspects can be found down 50-150 cm. in some parts of the region. No recent avalanches have been reported on these layers. 

Big warm ups can awaken dormant weak layers resulting in large avalanches. Steep, rocky, convex terrain with a shallow or thin to thick snowpack are examples of places where triggering these layers are more likely.

Sunshine and warm temperatures often cause large cornice failures which are hazardous on their own and can also trigger large avalanches on deeper weak layers that the weight of a single rider would not trigger.

Terrain and Travel

  • Avoid exposure to slopes that have cornices overhead.
  • Cornice failure may trigger large avalanches.
  • Back off slopes as the surface becomes moist or wet with rising temperatures.
  • Avoid steep, rocky, and wind effected areas where triggering slabs is more likely.

Problems

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.

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.

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.