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

Dec 28th, 2012–Dec 29th, 2012

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.
Below Treeline
Natural avalanches unlikely.

Regions

Jasper.

Continued loose snow avalanches on steep alpine and tree line slopes.  Be prepared for these sloughing on or under slopes and  ice climbs .

Weather Forecast

Light NW winds with the possibility of some light snow flurries can be expected on Saturday.  Cool overnight temperatures will warm to above seasonal values by the afternoon with sunny breaks.

Snowpack Summary

Moderate to strong SW winds have created slab conditions on open tree line slopes and along ridge lines in the alpine.  The mid-pack is facetting but remains strong where it is deeper than a meter.  In shallow areas, facetting has weakened it significantly.

Avalanche Summary

In the past 2 days, surface facets have created numerous small loose avalanches at tree line and above in the Icefields area.  These slides have little mass and have not as yet triggered the wind slabs beneath them.  No natural slab avalanches were observed today.

Confidence

Due to the number and quality of field observations on Saturday

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.