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Avalanche Forecast

Archived

Mar 5th, 2020–Mar 6th, 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

North Columbia.

It's complicated: 1) fresh snow may disguise reactive wind slabs; 2) a widespread, touchy weak layer may just be waiting for a trigger; 3) clearing skies in the afternoon could ramp up reactivity. 

Avalanches have been large and human triggering remains likely at all elevations.

Confidence

High -

Weather Forecast

Thursday night: Cloudy, 5-10 cm of snow, moderate southwest winds, alpine temperature -7 C,freezing level dropping to valley bottom.

Friday: Decreasing cloud, isolated flurries with trace accumulations, light southwest winds, alpine high temperature -2 C, freezing level 1100 m.

Saturday: Increasing cloud, up to 5 of snow, light variable winds, alpine high temperature -4 C, freezing level at valley bottom.

Sunday: Partly cloudy, 5-10 cm of snow overnight, light southwest winds, alpine high temperature -7 C, freezing level at valley bottom.

Avalanche Summary

Over the past several days, a natural wind slab avalanche cycle was observed. These avalanches were small to large (size 1-2.5) breaking 25-50 cm deep on leeward features at upper elevations. In several cases, cornice falls triggered these wind slabs. 

There has been a flood of reports of avalanches releasing on the February 22 surface hoar since Saturday. Both 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 since the weekend, 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 slabs stepping down in the alpine. This combination has produced very large (size 3-4) avalanches.

Snowpack Summary

Incremental snowfall and recent strong winds formed reactive wind slabs in the alpine and open areas at treeline that remain likely to human trigger. Convective showers in the wake of the storm may obscure the evidence of these wind slabs.

A weak layer of widespread surface hoar is buried 40-80 cm deep. It may sit over a crust on solar aspects. Incremental loading from successive storms, strong winds, and mild temperatures have strengthened the slab character and increased the depth of the snow above, creating the potential for larger avalanches with serious consequences. Read more about surface hoar on our forecaster blog!

Terrain and Travel

  • Avoid freshly wind loaded terrain features.
  • 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.
  • 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.

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.