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 17th, 2022–Jan 18th, 2022

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

Regions

Northwest Inland.

Watch for wind slabs in steep terrain features at high elevations.

Confidence

High - Confidence is due to a stable weather pattern with little change expected.

Weather Forecast

MONDAY NIGHT: Clear skies with no precipitation, 20 km/h northwest wind, alpine temperature -8 C.

TUESDAY: Partly cloudy with no precipitation, 10 km/h west wind, alpine temperature -10 C.

WEDNESDAY: Cloudy with snowfall, accumulation 5 cm, 50 km/h southwest wind, alpine temperature -10 C.

THURSDAY: Cloudy with snowfall, accumulation 5 to 10 cm, 50 km/h southwest wind, alpine temperature -6 C.

Avalanche Summary

Storm and wind slab avalanches were triggered naturally and by explosives on Sunday. They were small to large (size 1 to 2) and around 20 to 30 cm deep. At lower elevations, wet loose and wet slab avalanches were observed from rain.

Avalanche activity is anticipated to decrease on Tuesday with cooler and calm weather.

Snowpack Summary

Around 10 to 20 cm of recent snow fell above 1200 m. The snow has been redistributed by strong southwest to northwest wind, forming wind slabs in lee terrain features. The snow may overly surface hoar in areas sheltered from the wind. Below around 1200 m, the precipitation mostly fell as rain, which has frozen into a hard melt-freeze crust.

A weak layer of faceted grains is found about 30 to 60 cm deep, which formed during the cold spell in late December and early January. There is uncertainty in if and when this layer will become an avalanche problem, but until now we haven't seen substantial activity on it.

In thin snowpack areas, the base of the snowpack is composed of weak faceted grains around various melt-freeze crusts, which are considered dormant at this time.

Terrain and Travel

  • Be careful as you transition into wind affected terrain.
  • Avoid freshly wind loaded terrain features.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.