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 1st, 2017–Jan 2nd, 2017

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

Regions

North Columbia.

Watch for wind slabs in unusual places as we head into a clear cold week.

Confidence

High - The weather pattern is stable

Weather Forecast

MONDAY: Sunny, 10-20 km/h east winds, alpine temperatures around -20.TUESDAY: Sunny with cloudy periods, 10-30 km/h northeast winds, alpine temperatures around -20.WEDNESDAY: A mix of sun and cloud, 10-30 km/h northeast winds, alpine temperatures around -18.

Avalanche Summary

Several natural wind slabs were reported in the Selkirks and north Monashees on Sunday, typically in the size 2 range. Looking ahead to Monday, expect wind slabs to remain reactive to human triggers.

Snowpack Summary

The region received 50 to 100 cm of new snow between Christmas and New Years. This snow has been redistributed by strong winds that have come from a variety of directions and loaded leeward and cross-loaded features. Sunny skies this week will promote settlement of the snow on open south-facing slopes. The mid-December facet/surface hoar interface can be found buried 80-120 cm deep, and has been showing signs of gaining strength recently with little to no recent avalanche activity in the region. The layer may still be reactive in isolated areas such as steep south-facing slopes and thin snowpack areas in the northern and eastern parts of the region. The lower snowpack is well bonded and features a thick rain crust near the ground.

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.