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

Jan 16th, 2018–Jan 17th, 2018

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

Regions

Kananaskis.

Good skiing was found in sheltered areas.  We are in for a change.  Strong winds are expected until Thursday, thus creating wind slabs into tree line.  Snow on the way starting Wednesday night.

Confidence

High -

Weather Forecast

Wednesday is suppose to bring cloudy skies with isolated flurries.  55-80km/h SW winds are expected to start Tuesday night and continue through to Thursday.  Temperatures in the alpine for Wednesday should reach -4c.  Periods of snow are expected for Thursday.

Avalanche Summary

No new observed.

Snowpack Summary

Surface hoar is continuing to grow on the surface and could become an issue if Thursday snowfall is of great amounts. Some wind effect at tree line was observed.  Jan 6 SH layer is mostly found below 2200m and not much of a concern because of the lack of a slab.  The Dec 15 layer is variable in the alpine and more prominent at treeline.  The November crusts are starting to show some breakdown with more facets around the crust.

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.