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Avalanche Forecast

Archived

Apr 3rd, 2022–Apr 4th, 2022

Alpine
Natural avalanches possible, human triggered probable.
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.

Carefully assess the wind slab hazard as you gain elevation. Wind slabs could be touchy due to the underlying crust.

Confidence

Low - Uncertainty is due to the track & intensity of the incoming weather system.

Weather Forecast

Sunday night: light flurries bringing up to 5 cm of new snow with moderate south winds. Low of -3 at 2000 m.

MONDAY: Cloudy with 5 cm of new snow. Moderate south winds shifting to southwest in the late afternoon. Freezing level rising to 1900 m.

TUESDAY: A mix of sun and cloud with no new snow expected. Light to moderate west wind and freezing level around 1800 m.

Wednesday: Sunny with no new snow expected. Light west winds and freezing levels around 2000 m.

Avalanche Summary

In the past few days small wind slab avalanches have been triggered by skiers on north and east facing terrain in the alpine. On Saturday one natural cornice fall was observed, it did not trigger a slab on the slope below.

Snowpack Summary

Wind slabs may be found in exposed terrain in the treeline and alpine. A crust exists on or near the surface on all aspects as high as 2500 m. This crust will become moist at lower elevations as the freezing level rises. Multiple crusts exist on solar aspects.

Cornices have been observed throughout the region. Best practice is to limit time traveling on slopes below these hazards.

At 30 to 75 cm below the snow surface, a sun crust can be found on solar aspects from March. The recent warm weather seems to have helped this layer bond. 

A thick rain crust with facets above from early December is buried around 150 cm deep. Large avalanches were naturally triggered on this layer during the most recent warm temperatures in western terrain near the Bugaboos. Continued avalanche activity on this layer is unlikely with cooler temperatures forecast. 

Terrain and Travel

  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.