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Avalanche Forecast

Archived

Feb 15th, 2022–Feb 16th, 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

Sea To Sky.

The likelihood of triggering the late January layer is low but not impossible. Use extra caution on slopes where a thick supportive crust is absent.

Confidence

Moderate -

Weather Forecast

Tuesday night: Low of -4 at 1400m. Lightt to moderate northwest winds with the possibilities of light flurries bringing trace amounts of snow.

Wednesday: mostly sunny with freezing levels rising to 1600m. Light to moderate northwest winds. 

Thursday: Cloudy with light flurries bringing trace amounts of snow. Light to moderate northwest winds and freezing levels rising to 1300m.

Friday: cloudy with the possibility of light flurries bringing trace amounts of snow. Light to moderate northwest winds and freezing levels rising to 1300m.

Avalanche Summary

On Sunday, several natural cornices were observed in the north of the region, some of which triggered size 1-2 slabs on the slopes below. Small loose wet avalanches were also observed from steep sun-exposed slopes. 

On Saturday, a natural size 2 cornice release was reported from a steep, rocky NW aspect at 2100 m. A variety of loose wet avalanches were reported from steep, sun-exposed slopes. Explosives triggered four cornices up to size 2. 

Snowpack Summary

A dusting of new snow has buried a widespread surface crust and wind-affected surfaces in exposed high elevation terrain. The new melt-freeze crust is reported to exist on all aspects and elevations except for some of the highest elevation polar aspects which may still hold dry snow. The crust is reported to be undergoing faceting in some areas.

The late-January crust/facet/surface hoar interface is buried down 30-70 cm. This layer was most reactive between 1700 m and 2000 m. While this layer now appears to be dormant in many parts of the region, recent snowpack tests suggest it is still very reactive in a few places and would still be capable of producing large avalanches if triggered. 

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of buried persistent weak layers.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.