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 17th, 2013–Mar 18th, 2013

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

Regions

South Rockies.

Confidence

Fair - Forecast snowfall amounts are uncertain on Monday

Weather Forecast

Monday: Light snow (5-10 cm). Moderate W to NW winds. Alpine temperature near -9.Tuesday: No snow. Light W winds. Alpine temperature near -6.Wednesday: Light snow. Light to moderate SW winds. Alpine temperature near -4.

Avalanche Summary

Observations were limited during Sunday's storm, but it's suspected that some natural activity occurred in response to rapid snow loading.

Snowpack Summary

20-30 cm snowfall on Sunday landed on a crust above about 2000 m, or moist snow at lower elevations. Ridge top winds have been from SW and NW directions, creating wind slabs on a variety of lee and cross-loaded slopes. Deeper in the snowpack, a series of crust layers makes up the upper snowpack. The mid-pack is reported to be generally well-settled. Cornices are large and fragile in some areas.

Problems

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.

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.