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 11th, 2020–Jan 14th, 2020

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

Regions

Waterton Lakes.

Recently created windslabs will become difficult to spot as the Waterton receives a moderate amount on low density snow over the next few days. If triggered, windslabs may step down to the late December melt freeze crust.

Weather Forecast

Sunday: 5-10cm overnight. Cloudy with scattered flurries during the day. Total daytime accumulation 5-10cm. Light SE Winds. Temperature dropping rapidly overnight.

Monday: Continued extreme cold with flurries totalling 5 cm. Moderate NE winds

Tuesday: Extreme cold with flurries.

Snowpack Summary

Extreme West winds yesterday have created a 10-60cm windslab sitting low in start zones on all but W aspects. New snow on top of this windslab produce small loose dry avalanches. A crust down 20-70cm exists up to 1800m. The middle snowpack is well settled in deep snowpack areas but a weak facet/ melt freeze crust still lurks at base of snowpack.

Avalanche Summary

No new avalanches observed.

Confidence

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 Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.