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Avalanche Forecast

Archived

Mar 7th, 2020–Mar 8th, 2020

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

Regions

Cariboos.

Sunny breaks after a week of storms may make wind slabs and cornices more sensitive to failure. A buried weak layer warrants a conservative mindset and terrain use strategy, particularly in the south of the region. Where this layer is absent, danger ratings may be a step lower.

Confidence

Moderate - Uncertainty is due to extremely variable snowpack conditions reported through the region.

Weather Forecast

Saturday night: Clearing overnight, light variable winds, alpine temperature -15 C..

Sunday: Mix of sun and cloud, light west winds, alpine high temperature -7 C.

Monday: Mostly clear, light southwest winds, alpine high temperature -5 C, freezing level 1000 m.

Tuesday: Increasing cloud, 5-10 cm of snow, moderate to strong south winds, alpine high temperature -4 C, freezing level 1300 m.

Avalanche Summary

Over the past several days, a natural cycle of large to very large (size 2-3) avalanches released in the recent storm snow, primarily on wind-loaded aspects (northeast, east, and southeast) above 1800 m. Several were triggered by large cornices failures. If triggered, wind slabs and cornices could step down to the buried surface hoar layer, forming large avalanches. Use added caution on sun-exposed slopes when the sun is shining, as it could rapidly deteriorate the storm snow and cornices and cause loose or slab avalanches.

Many large to very large avalanches (size 2-3) releasing on the February 22 surface hoar have been observed over the past week. These avalanches primarily occurred on north, northeast, and east aspects between 1400-2100 m and in the southern part of the region. These avalanches have propagated widely across terrain features, warranting conservative terrain margins. Check out this MIN reporting a large, snowmobile-triggered avalanche on Friday for a helpful example. 

Snowpack Summary

Incremental snowfall and wind have formed reactive wind slabs in the alpine and open areas at treeline that remain possible to human trigger. Cornices are large and looming after a week of successive storms.

A weak layer of surface hoar may be found 60-100 cm deep. There is uncertainty about the distribution and reactivity of this layer, especially in the north of the region. This MIN from the Trophy Mountains and this MIN from Allan Creek confirm the presence of this layer in the southern half of the region. Sheltered north, northeast, and east facing slopes near treeline are the most suspect. Riders will be capable of triggering this layer for some time until there is a substantial change in the snowpack. Read more about surface hoar on our forecaster blog.

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Use conservative route selection and resist venturing out into complex terrain.
  • Stay off recently wind loaded slopes until they have had a chance to stabilize.
  • Even brief periods of direct sun could produce natural avalanches.

Problems

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.

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.