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 10th, 2018–Jan 11th, 2018

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

Northwest Coastal.

Potential for a cold, windy day. Watch for building wind slabs, even at low elevation.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

THURSDAY: Cloudy with strong outflow winds. Flurries possible. Alpine temperature near -20.FRIDAY: Clear with light winds. Flurries possible. Alpine temperature near -20.SATURDAY: Cloudy with light winds. 5-10 cm snow. Alpine temperature near 0, but cold in the valleys.

Avalanche Summary

A natural storm slab cycle to size 2 was reported to have run during the storm last Monday. Skiers near Shames reported sluffs running far on Monday. A skier triggered a size 2 wind slab on Sunday on a NW aspect at about 1400 m near Terrace.

Snowpack Summary

The snowpack is variable across the region. Wind slabs and storm slabs may be found on some slopes in the alpine and at treeline. Up to 45 cm recent snow overlies several layers of interest in the upper snowpack. These include crusts, surface hoar and facets. A hard crust with associated facets from mid-December sits deeper in the snowpack, about 60 cm down. Any of these layers could create a persistent slab problem if new snow, wind-loading or warming change the properties of the slab above.The lower snowpack is generally strong, with the exception of areas around Stewart and further north where a basal crust and facets exist.

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.