Avalanche Forecast

Wednesday night: Clear with cloudy periods and isolated flurries, moderate northwest wind, alpine high temperature -10 C, freezing level at valley bottom.

Thursday: Mix of sun and cloud with isolated flurries, light west wind, alpine high temperature -10 C, freezing level at valley bottom. 

Friday: Mostly cloudy, 5-15 cm of snow, moderate northeast wind, alpine high temperature -10 C, freezing level at valley bottom.

Saturday: Mostly cloudy with isolated flurries, moderate northeast wind, alpine high temperature -20 C, freezing level at valley bottom.

Numerous wind slab and storm slab avalanches up to size 2 were triggered naturally and by humans on Tuesday and released on the old snow surface which was covered by 20-40 cm of recent storm snow.

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

Reports of large (size 2-3) human, remotely and explosive-triggered avalanches releasing on the February 22 surface hoar layer continued throughout the weekend and into Tuesday 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+.

The recent storm delivered 20-40 cm of snow with strong southwest winds. The new snow is not expected to bond well with previous surfaces. Strong winds built slabs on lee features at upper elevations, where southwest winds transported the snow into deeper, more cohesive drifts.

A widespread weak layer of surface hoar is buried 60-120 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.

• Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
• 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.
• Minimize your exposure time below cornices.