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Avalanche Forecast

Archived

Mar 10th, 2020–Mar 11th, 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 unlikely, human triggered possible.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

South Columbia.

New snow overnight will increase storm snow totals to 25-45 cm. Strong westerly wind will build slabs which will be reactive to human triggering especially in lee terrain features. A buried weak layer warrants a conservative mindset and terrain use strategy.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

Tuesday night: Cloudy, 15-25 cm snow, strong westerly wind, alpine high temperature -6 C, freezing level 1200 m.

Wednesday: Mostly cloudy with isolated flurries, moderate northwest wind, alpine high temperature -7 C, freezing level 1000 m. 

Thursday: Mix of sun and cloud with isolated flurries, light westerly wind, alpine high temperature -7 C, freezing level 900 m. 

Friday: Mostly cloudy, scattered flurries with up to 5 cm snow accumulation, moderate easterly wind, alpine high temperature -10 C, freezing level at valley bottom.

Avalanche Summary

A few natural and human triggered storm slabs up to size 2 were reported on Monday.

Reports of large (size 2-3) human-triggered and remotely-triggered avalanches releasing on the February 22 surface hoar layer continued throughout the weekend into Monday from operators region-wide. This layer continues to surprise people with remote-triggered activity, wide propagation, and a false sense of stability from unreactive ski cuts or from multiple people moving through the terrain before an avalanche releases. Observations have extended to all aspects and elevations, but north to east aspects near treeline have been a hot-spot for reactivity. Avalanches have also occurred at unusually high elevations for surface hoar, with several cases of wind slabs stepping down in the alpine. While the number of reported avalanches has decreased, the size has increased, with more of the activity releasing size 2+.

New snow and wind on Tuesday may have built reactive storm slabs and add a new load to cornices. Shallow storm slab avalanches or cornice falls have the potential to step-down to deeper layers and produce very large avalanches. 

Snowpack Summary

A storm moved into the region on Tuesday and is expected to bring 25-45 cm of snow with strong westerly winds by Wednesday morning. The new snow is not expected to bond well with previous surfaces. Expect the new snow to develop slabs on lee features at upper elevations, where westerly winds transport the snow into deeper, more cohesive drifts. 

A widespread weak layer of surface hoar is buried 50-90 cm deep. On solar aspects, this layer may sit over a crust. This persistent slab problem is transitioning into a low probability/high consequence scenario. The snow above the weak layer has increased in depth and slab properties, making avalanches more difficult to trigger and masking obvious clues that the problem is present (i.e. cracking, whumpfing). However, if triggered, avalanches will be large and getting caught could have serious consequences. Managing this problem requires a patient and diligent mindset, implemented by avoiding suspect slopes and maintaining conservative terrain margins. This persistent weak layer will likely pose the threat of a low probability/high consequence avalanche until there is a substantial change in the snowpack. Read more about surface hoar on our forecaster blog.

Terrain and Travel

  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Dial back your terrain choices if you are seeing more than 20 cm of new snow.
  • Be aware of the potential for large avalanches due to the presence of buried surface hoar.
  • If triggered, storm slabs in-motion may step down to deeper layers and result in very large avalanches.

Problems

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.

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.