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

Mar 28th, 2018–Mar 29th, 2018

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

Jasper.

The Icefields Parkway is planned to be closed at 2pm Thursday for avalanche control from Athabasca Falls to Saskatchewan crossing. Please plan accordingly.

Weather Forecast

Thursday will be cloudy and flurries, 5cm of snow, High of -6 and 15-40km/hr SW winds. Friday will be 12cm of snow, -18 to -6 degress Celsius, and light to 45km/hr West winds. Saturday will be sun and cloud, no precipitation, Alpine temperature Low -20 C, High -8 C, light ridge wind.

Snowpack Summary

Wind slabs and extensive wind effect is found in open areas. The upper snowpack is a windslab up to 50cm thick that sits on a sun-crust on solar aspects and facets on polar aspects. In many location the snowpack is facetted yet switching to spring snowpack conditions slowly.

Avalanche Summary

Wednesday's road patrol noted one size 3 noted in Maligne area, likely 3+ days old. Icefield's area noted one size 3 on the Mt Athabasca ramp, and one size 2.5 from a W aspect.

Confidence

Timing, track, or intensity of incoming weather system is uncertain on Thursday

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.