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Avalanche Forecast

Archived

Mar 7th, 2020–Mar 8th, 2020

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 possible, human triggered probable.
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.

Regions

South Columbia.

The snowpack cannot be trusted right now. Large, human-triggered avalanches on a buried weak layer continue across all aspects and elevations. Signs of the problem are becoming less obvious while the consequences are becoming more serious. Keep it conservative on Sunday.

Confidence

Moderate - Uncertainty is due to the fact that persistent slabs are particularly difficult to forecast.

Weather Forecast

Saturday night: Decreasing cloud, isolated flurries with trace accumulations, light west wind, alpine temperature -8 C.

Sunday: Mostly cloudy, convective flurries with up to 5 cm of snow, higher accumulations possible in the south of the region, light west winds, alpine high temperature -4 C, freezing level 800 m.

Monday: Mostly clear, light southwest winds, alpine high temperature -3 C, freezing level 1100 m.

Tuesday: Increasing cloud, 5-10 cm of snow, moderate southwest winds, alpine high temperature -3 C, freezing level 1200 m.

Avalanche Summary

Consistent reports of avalanches releasing on the February 22 surface hoar have been submitted over the past week. Human-triggered and remotely-triggered avalanches have been reported by nearly every operation region-wide, even as professionals tiptoe around and avoid suspect terrain features. The problem is touchy but tricky. In many instances, slopes were ski cut with no results, only to have the third or fourth skier in the group trigger the slab. Avalanche size has increased over the past week, with more of the activity releasing size 2+. Observations extend to all aspects and elevations, but north to east aspects near treeline have been a hot-spot for reactivity. 

Avalanches are also occurring at unusually high elevations for surface hoar, with several cases of wind and storm slabs stepping down in the alpine. Shallow avalanches in the most recent storm snow have the potential to step-down this deeper layer. Use added caution on sun-exposed slopes when the sun is shining, as it could rapidly deteriorate the storm snow and cornices and cause loose or slab avalanches.

Snowpack Summary

Snowfall amounts varied across the region on Saturday, with the highest totals falling in the southern part of the region. Areas that accumulated more than 20 cm may have formed a storm slab problem prone to human triggering. In areas where less snow accumulated, slab formation will likely be specific to where the wind has transported the snow into deeper drifts. 

A widespread weak layer of surface hoar is buried 50-90 cm deep. On solar aspects, this layer may sit over a crust. Incremental loading from successive storms, strong winds, and mild temperatures have increased the depth and slab properties of the snow above the weak layer, increasing the potential for larger avalanches with more serious consequences. Riders will be capable of triggering this layer for some time until there is a substantial change in the snowpack. Read more about surface hoar on our forecaster blog.

Terrain and Travel

  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Use conservative route selection and resist venturing out into complex terrain.
  • Storm slabs in motion may step down to deeper layers resulting in large avalanches.
  • Even brief periods of direct sun could produce natural avalanches.

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.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.