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Avalanche Forecast

Archived

Feb 4th, 2022–Feb 5th, 2022

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

Sea To Sky.

Avoid avalanche terrain at treeline where triggering the current persistent slab problem is most likely. Remote triggering is possible, always know whats above you.

Confidence

Moderate -

Weather Forecast

Friday night: Flurries with winds shifting to moderate from the northwest. Low of -2 at 1400 m.

Saturday: Light flurries in the morning with moderate northwest winds. Freezing level rising to 2000 m.

Sunday: sunny with No new snow expected. Moderate southwest winds and freezing levels rising to 2000 m.

Monday: stormy weather with up to 10 cm of snow and moderate to strong southwest winds. Freezing levels around 1300 m.

Avalanche Summary

Over the past few days several skier triggered avalanches to size 2 have been reported. We believe these avalanches have been failing on the same layer, a layer of facets on a crust from late January. Most avalanche activity on this layer is around 1900m but some have been reported in the alpine as well.

On Tuesday, we received report of a large (size 2.5) human-triggered avalanche near Rainbow Mountain that caught and carried a group of five skiers. The avalanche released on a north aspect at 1900 m. It broke 40 cm deep and ran on the late January facet-crust layer. The avalanche propagated across adjacent roll-over features and triggered a sympathetic slide on a small feature 200 m away.

Snowpack Summary

15 cm of new snow with moderate to strong southwest winds will have formed wind slab on north and east aspects on Friday.

A layer of facets on a crust is now buried down 40 to 70 cm. This layer is widespread between 1800 m and 2000 m, but could be found above and below this elevation band. It has produced several human and remote triggered avalanches in the past few days. In sheltered terrain at treeline surface hoar can also be found on this layer.

Deeper in the snowpack, it is possible to find another crust layer buried down 100-200 cm with facets above it from December. This layer is most prominent between 1700-2100 m and is currently classified as dormant; although large loads such as a cornice failure or avalanches in motion may still be able to trigger avalanches on this layer.

Terrain and Travel

  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Be aware of the potential for large avalanches due to the presence of buried weak layers.
  • Remote triggering is a concern, watch out for adjacent and overhead slopes.
  • Extra caution is needed around cornices under the current conditions.

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.