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Avalanche Forecast

Archived

Mar 8th, 2022–Mar 9th, 2022

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

Regions

Purcells.

Check your line for isolated pockets of wind slab at upper elevations. Though stability is improving, it remains possible to trigger avalanches on a recently buried weak layer, especially with large loads like cornice failures.

Confidence

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

Weather Forecast

Tuesday night: Flurries bringing up to 5 cm. Light easterly wind. Alpine low around -18 °C.

Wednesday: Sunny. Light easterly wind. Alpine temperatures around -14 °C.

Thursday: A mix of sun and cloud. Light to moderate west wind. Alpine temperatures around -10 °C.

Friday: A mix of sun and cloud. Light to moderate west wind. Alpine high around -3 °C. Freezing level rising to 1400 m.

Avalanche Summary

Human triggered avalanche activity has largely tapered off since Friday when several riders triggered storm slabs and loose dry avalanches in the recent snow, including this remotely triggered size 1.5 near Golden.

Solar triggered avalanche activity has been ongoing since the weekend. Countless loose dry avalanches up to size 1.5 have been reported out of steep or extreme terrain throughout the region as well as a few cornice failures up to size 3. Cornices and loose dry avalanches have also served as triggers for slabs on slopes below, including a size 2 reported on Tuesday near Invermere.

Warm temperatures Thursday through Sunday are suspected to have sensitized buried weak layers such that large explosives were able to trigger a few deep avalanches:

  • On Sunday explosive work near Panorama triggered size 1.5-2 avalanches on a buried weak layer from mid February up to 40 cm deep. Another round on Monday produced size 1-1.5s on the same layer but showing less propagation. 
  • On Friday in the Bugaboos, large explosives triggered several very large avalanches, mostly on northerly aspects in the alpine, including one size 3.5 with a crown 60-200 cm deep.
  • Check out this MIN report from Golden of a mysterious size 2 slab avalanche around treeline, suspected to have slid on the mid February weak layer.

Snowpack Summary

Surface snow has likely seen some redistribution and reverse-loading by recent wind in the alpine. These soft wind slabs may sit over recently formed crusts on solar aspects and below 1500 m.

In the south of the region, a well bonded rain crust may be found within the top 30 cm up to 1700 m. A more widespread recently buried weak layer sits 30-60 cm deep throughout the region. It consists of surface hoar in shady, wind-sheltered areas and a sun crust on solar aspects.

An interface from mid-February composed of sun crust and/or surface hoar is now 30-90 cm deep. Explosive work near Invermere (where it is less than 60 cm deep) on Sunday confirmed that this layer can still be triggered by large loads.

A layer of surface hoar from late January has not produced recent avalanche activity but crystals can still be identified 40-50 cm deep near Golden.

Terrain and Travel

  • Avoid exposure to slopes that have cornices overhead.
  • Recent new snow may be hiding windslabs that were easily visible before the snow fell.
  • Be careful with wind loaded pockets, especially near ridge crests and roll-overs.
  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.

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.

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.