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 6th, 2012–Jan 7th, 2012

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

Regions

South Columbia.

Confidence

Fair - Forecast snowfall amounts are uncertain on Sunday

Weather Forecast

Flurries during the day on Friday should accumulate a couple of new cm by Saturday morning. A weak ridge of high pressure building over the coast is forecast to develop strong winds from the west or northwest and warm temperatures in the Cariboo. Moderate precipitation is expected to begin by midnight and continue during the day on Sunday. The freezing level is expected to rise to about 1800 metres in the Cariboo and West Monashee by Sunday morning. It looks like most of the snow will fall in the North and West of the Interior ranges. Expect moderate to strong northwest winds on Sunday becoming strong from the west in the South Columbia and Purcells. Cooler air is expected to move in to the region from the northwest on Monday. Precipitation amounts are un-certain at this time. Chinook conditions are expected for the Rockies.

Avalanche Summary

Explosives control along the highway corridor in the Selkirks has been producing very large avalanches up to size 4.0. Some smaller natural avalanches releasing in the recent wind transported snow have been reported up to size 2.0. Reports have been limited due to poor visibility and travel conditions.

Snowpack Summary

The recent snow has been quite variable in it's distribution, depositing between 30-50 cm depending on the drainage. Generally it has been drier in the south of the region. Some areas have enough new snow for a "storm" slab to be reactive. The wind has been strong across the region, transporting snow onto north and east aspects. Windslabs have been touchy and releasing with wide propagations, sometimes stepping down to the mid-december surface hoar layer. Some areas have developed a rain crust after the recent warm temperatures that exists up to about 1600 metres.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.