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Avalanche Forecast

Archived

Dec 6th, 2020–Dec 7th, 2020

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

Kootenay Boundary.

Keep an eye out for rogue pockets of wind slab. Getting knocked off your feet can be serious in extreme terrain.

Confidence

Moderate - Uncertainty is due to the limited number of field observations.

Weather Forecast

SUNDAY NIGHT: Patchy clouds / Light, southwest ridgetop wind / alpine low temperature -7 / Freezing level valley bottom

MONDAY: Partly cloudy with isolated flurries / Light to moderate, southwest ridgetop wind / alpine high temperature -3 / Freezing level 1200 m, light inversion

TUESDAY: Cloudy with scattered flurries, 5-10 cm / Light, gusty southwest ridgetop wind / alpine high temperature -4 / Freezing level 1100 m

WEDNESDAY: Cloudy with scattered flurries, 5-10 cm / Light, gusty southwest ridgetop wind / alpine high temperature -4 / Freezing level 1000 m

Avalanche Summary

Outside of a few small loose-wet avalanches from steep terrain, there have been no avalanche observations since last Wednesday (Nov 2) when numerous wet loose avalanches were reported from NE slopes above 2000 m, likely triggered by warming.

Have you been out and about in the mountains? If so please submit to the Mountain Information Network (MIN). It doesn't have to be technical it can be as simple as a photo. Photos are especially helpful! Sending a big thank you to the already submitted MIN's this season!

Snowpack Summary

A melt-freeze crust covers most solar slopes and a variety of wind-affected surfaces around found on more polar slopes at treeline and above. Widespread surface hoar growth has been observed around the region. The snowpack is well settled below. Snowpack depths vary with elevation, treeline averages between 50-100 cm. 

Crusts from mid-and early-November are generally found 30 cm below the snow surface and 10 cm up from the ground at all elevations. While they are showing resistant planar results in snowpack tests, a lot of uncertainty still exists with limited observations.

Terrain and Travel

  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.
  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Small avalanches can have serious consequences in extreme terrain. Carefully evaluate your line for wind slab hazard before you commit to it.

Problems

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.