Avalanche Forecast

Moderate - Forecast snowfall amounts are uncertain.

Monday night: Mostly clear, light west wind, alpine high temperature - 12 C. 

Tuesday: Cloudy, 3-8 cm of snow, moderate southwest winds gusting strong at ridge-top, alpine high temperature -5 C, freezing level 1300 m.

Wednesday: Mostly cloudy, 5-10 cm of snow, light northwest winds, alpine high temperature -4 C, freezing level 1300 m. 

Thursday: Mostly cloudy, isolated flurries with trace accumulations, light west winds, alpine high temperature -6 C, freezing level 800 m.  

Over the weekend, a natural storm slab avalanche cycle was observed. These avalanches were small to large (size 1-2.5) and breaking 20-40 cm deep. Shallow slabs in the recent snow have the potential to step down to the buried surface hoar layer, creating very large avalanches. 

Over the past week, human-triggered avalanches releasing on the February 22 surface hoar have been consistently reported. In many instances, slopes were ski cut with no results, only to have the third or fourth skier in the group trigger the slab. These avalanches have been remotely-triggered and have propagated widely across terrain features, warranting conservative terrain margins (see this MIN for a helpful example). Observations extend to all aspects and elevations, but north to east aspects near treeline have been a hot-spot for reactivity. 

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 the deep persistent slab problem remains a concern. 

Snowfall amounts from the weekend storm ranged from 20-40 cm. Human triggering remains possible where the wind has transported the snow into deeper drifts. Incremental snowfall and wind forecast for Tuesday is expected to add to this wind slab problem.

A weak layer of surface hoar from February 22 may be found 35-70 cm deep. It may sit over a crust on solar aspects. With successive storms, more areas have reached critical loading and developed a slab over this layer. 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 remain a problem until there is a substantial change in the snowpack. 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.

• 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.
• Stay off recently wind loaded slopes until they have had a chance to stabilize.
• Avoid shallow, rocky areas where the snowpack transitions from thick to thin.