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Avalanche Forecast

Archived

Mar 6th, 2020–Mar 7th, 2020

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

Regions

Purcells.

The snowpack is not to be trusted. Reports of large, human-triggered avalanches on a buried weak layer continue across aspects and elevations. Keep it conservative on Saturday. Where more than 20 cm of snow accumulates, expect avalanche danger to be HIGH.

Confidence

Moderate - Uncertainty is due to the track & intensity of the incoming weather system.

Weather Forecast

Friday night: Cloudy, 5-10 cm snow, light south wind, alpine temperature -4 C.

Saturday: Cloudy, 5-15 cm new snow, light southwest wind, alpine high temperature -4 C, freezing level 1000 m.

Sunday: Mostly cloudy, scattered flurries with up 5 cm of snow, light southwest winds, alpine high temperature -5 C, freezing level 1000 m.

Monday: Mostly clear, light southwest wind, alpine high temperature -4 C, freezing level 1200 m. 

Avalanche Summary

Over the past week, large (size 2-2.5) persistent slab avalanches have been observed where the most snow has accumulated over a layer of surface hoar. Human, machine, and remotely-triggered avalanches have all been reported, 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 accidentally trigger the slab. 

Over the past several days, small to large (size 1-2) natural, human-triggered, and explosive-triggered avalanches have been observed breaking in the recent storm snow. A few large (size 2) cornices were also observed failing naturally. With incoming snow overnight, a new touchy storm slab problem may form on the surface, increasing the potential for cornices to reach their breaking point and creating conditions where shallow avalanches have the potential to step-down to deeper layers. 

On Thursday, professionals reported large (size 2.5) explosive triggered avalanches releasing on weak layers near the ground. These avalanches occurred on north and east facing slopes above 2300 m, and they confirm that this problem remains a concern. 

Snowpack Summary

An incoming storm is expected to bring up to 20+ cm of snow to the region by afternoon on Saturday. Snowfall amounts are expected to vary across the region. Areas that accumulate more than 20 cm may develop a touchy storm slab problem.

A weak layer of surface hoar sits 35-70 cm deep. It may sit over a crust on solar aspects. With snow in the forecast, more areas are expected to reach critical loading and slab formation over this layer. The problem will likely become more reactive and widespread. Read more about surface hoar on our forecaster blog!

Deep basal facets lurk near the bottom of the snowpack. This layer has been responsible for sporadic deep persistent slab avalanches, usually triggered from shallow, rocky start zones.

Terrain and Travel

  • Conservative terrain selection is critical, choose only well supported, low consequence lines.
  • Watch for fresh storm slabs building throughout the day.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.

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.