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 3rd, 2013–Jan 6th, 2013

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

Waterton Lakes.

Good skiing in sheltered areas today with easy travel conditions! Cornice hazard and wind slabs remain the main avalanche concerns over the next few days.

Weather Forecast

The ridge of high pressure will break down over the next several days as a more zonal Westerly flow becomes established. Temperatures remain moderate and seasonal.  Winds will stay in the moderate to strong range especially over Eastern areas of the park. Some light precipitation may be possible on Sunday. 

Snowpack Summary

Some surface hoar growth over the last two days at all elevations.  Light sun crust on steep S aspects.  Moderate W winds creating hard and soft wind slabs in open areas at tree line and in the alpine.  Below this the snowpack is generally well settled with no major shears.  Still some concerns for weak basal facets in shallow snowpack areas.

Avalanche Summary

No new avalanche activity over the past two days.  We did see several avalanches up to size 3 out of steep wind loaded alpine terrain a few days ago.  These appeared to be cornice triggered and failing on deeper buried facet layers.  This remains a concern especially in areas where the snowpack depth varies substantially. 

Confidence

Wind effect is extremely variable

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.