Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 2nd, 2022–Feb 3rd, 2022

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

Regions

Sea To Sky.

Carefully assess for the presence of a persistent weak layer before committing to a slope. If in doubt choose simple terrain.

Confidence

Low - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Wednesday night: light snow and moderate west winds. Low of -8 at 1400m.

Thursday: light flurries and light to moderate west winds. Freezing level rising to 1000m.

 

Friday: stormy with 10cm of new snow.Strong southwest winds with extreme gusts. Freezing level rising to 1400m.

Saturday: light flurries with moderate northwest winds. Freezing level rising to 1400m.

Avalanche Summary

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 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. 

A skier remote size 2 was also observed on a northeast aspect at 1900m on Tuesday. This avalanche released on the same layer from late January.

On Monday, operators reported numerous large (size 2-2.5) human and explosive-triggered avalanches breaking 20-50 cm deep in the recent storm snow. In a few areas, these slabs broke 70-100 cm deep. In the backcountry, a group remotely triggered an avalanche from Panorama Ridge on a northeast aspect in the alpine. Near Gin Peak, a skier was caught and carried in a small avalanche that released on a steep, convex feature at treeline. On Sunday, a group also travelling near Gin Peak reported triggering a small (size 1.5) avalanche. The avalanche was triggered remotely from below and broke 50 cm deep. 

Last week, explosive control work near Whistler produced a cornice fall that triggered a size 2.5 deep persistent slab on the weak faceted crystals above the early December crust. The slab broke 60-130cm deep. This indicates that while the weak layer is unlikely to be affected by skiers and riders, it could still be triggered by very large loads. 

Snowpack Summary

Winds have varied in direction over the past few days redistributing up to 50cm of recent storm snow into wind slabs on all aspects. The recent snow rests on a problematic layer combination. Weak sugary facets formed during a prolonged dry period over a thick melt-freeze crust. In sheltered areas at upper elevations, surface hoar may also be found on the crust. This late January facet-crust layer has demonstrated continuing reactivity in the aftermath of the weekend storm. Travelers have reported remote-triggered avalanche activity, widespread whumpfing on this layer (see this report from Paul Ridge), and reactivity in snowpack tests (see this report from Gin Peak). 

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

  • Recent wind has varied in direction so watch for wind slabs on all aspects.
  • 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

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.