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Avalanche Forecast

Archived

Dec 5th, 2018–Dec 6th, 2018

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

Cariboos.

Field observations are very limited in the Cariboos. It is important to supplement this forecast with your own observations. If you get out into the mountains, tell us what you see by posting to the Mountain Information Network! (MIN)

Confidence

Moderate - Due to the number of field observations

Weather Forecast

WEDNESDAY NIGHT - Cloudy with clear periods / light southerly winds / alpine low temperature near -11THURSDAY -Sunny with cloudy periods / light southerly winds / alpine high temperature near -7FRIDAY - A mix of sun and cloud / light to moderate southerly winds / alpine high temperature near -5, low temperature near -5. Some areas will experience an alpine temperature inversion.SATURDAY - Cloudy with sunny periods and isolated flurries / light to moderate south winds / alpine high temperature near -4, low temperature near -8

Avalanche Summary

No new avalanches have been reported.

Snowpack Summary

The primary concern in the snowpack is a weak layer of surface hoar (feathery crystals) and sun crust on steeper south facing slopes. This layer is down 30-60 cm. The surface hoar is most prominent at treeline, but it may exist in sheltered alpine areas.At the base of the snowpack is a crust that formed in late October. There have been no reports of reactivity on this layer in the Cariboos, however it may be reactive in isolated locations such as steep, rocky terrain, with a shallow snowpack. Snowpack depths decrease dramatically with elevation.

Problems

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.