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

Nov 7th, 2016–Nov 8th, 2016

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

Regions

Kananaskis.

Watch for early season hazards, such as shallow buried rocks and trees. Unusually high freezing levels expected.

Confidence

Moderate - Freezing levels are uncertain

Weather Forecast

Warm and windy for the next few days. Freezing levels will rise to mountain top on Tuesday. No precipitation expected.

Avalanche Summary

Nothing new observed or reported in past 24hrs.

Snowpack Summary

Early season conditions exist with snow only really in the Alpine elevation band. Wind slabs are found in lee features and gullies in the Alpine. Moist snow on solar aspects in the afternoon.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.