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 25th, 2015–Feb 26th, 2015

Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

South Columbia.

If warming persists, there will be a higher likelihood of avalanche activity, especially on steep, sun-exposed slopes.Are you a member of Avalanche Canada? Join today at avalanche.ca/membership

Confidence

Good

Weather Forecast

The ridge of high pressure will break down somewhat allowing for overcast skies and very light snowfall on Thursday and Friday. By Saturday the ridge will rebuild in all its glory bringing mainly sunny skies for the weekend. Freezing levels will hover around 1000m for the forecast period, with ridge top winds remaining mainly light from the northwest.

Avalanche Summary

With the warm temperatures on Monday, fairly widespread loose wet avalanche activity to size 2 was observed in sun-exposed terrain. Under the warm skies, a size 3 glide crack avalanche was also observed. In the North Columbia region, there was also some persistent slab avalanche activity on sun-exposed alpine slopes to size 3.5. With the forecast cooling trend, avalanche activity of this nature should taper-off.

Snowpack Summary

At higher elevations, up to 10 cm of wind-pressed snow overlies the previous variable snow surface of surface hoar, crusts, or wind affected snow depending on aspect and elevation. The "Valentine's Day" crust is just below the surface and is now strong and thick in most places. Thin isolated wind slabs may still be reactive in high elevation lee terrain, and cornices remain large and weak. The late-Jan crust/surface hoar layer (up to 100 cm deep) and the mid-January surface hoar (80-120 cm deep) are generally dormant, and chances of triggering these weaknesses have decreased. However, triggering may be possible with a large input such as cornice fall, or an avalanche stepping down, especially on sun drenched slopes.

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.