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 23rd, 2021–Jan 25th, 2021

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

Regions

North Rockies.

Keep hunting for sheltered snow to avoid lingering wind slab hazards and to find the best skiing and riding conditions.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

SATURDAY NIGHT: Cloudy with isolated flurries and a trace of new snow. Light west winds.

SUNDAY: Cloudy with scattered flurries bringing under 5 cm of new snow. Light southwest winds. Alpine high temperatures around -13.

MONDAY: Cloudy. Light southwest winds. Alpine high temperatures around -12.

TUESDAY: Cloudy. Light southeast winds. Alpine high temperatures around -13.

Avalanche Summary

On Tuesday, our field team reported widespread wind effect at all elevations, creating fragile cornices and reactive wind slabs on north and east facing slopes below ridgetops. MIN report HERE. Reports since that time have highlighted widespread wind effect throughout the region.

On Monday our field team observed some size 2 natural avalanches on a north facing alpine feature east of Crescent Spur. These likely ran over last weekend.

Snowpack Summary

30-50 cm of recent snow and extreme southwest winds have created large, fragile cornices and widespread wind effect in many locations, even open areas below treeline.

Underneath this snow you are likely to find a hard melt-freeze crust that can be found up to about 1600 m. You may also find a weak layer of buried surface hoar in isolated, sheltered locations below treeline. There is some concern for slabs reacting to the weight of a person or machine on steep slopes where this buried surface hoar exists. 

Around 60 to 130 cm of snow rests above another weak layer buried in early-December. On Jan 14th our field team found it in the Holmes area. Depending on location, the buried weak layer is composed of surface hoar and/or a crust/facet combination. Reports suggest that this layer has become dormant in much of the region except perhaps for the Pine Pass area.

Terrain and Travel

  • Carefully evaluate steep lines for wind slabs.
  • Avoid exposure to slopes that have cornices overhead.

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.