Avalanche Forecast

Low - Uncertainty is due to the complexity of the snowpack’s structure. Uncertainty is due to the speed, direction, or duration of the wind and its effect on the snowpack. Uncertainties in both the snowpack structure and the weather forecast limit our confidence.

The forecast period is marked by small amounts of snow, strong southwest wind and rising mid-week temperatures.

MONDAY NIGHT: Freezing level around valley bottom, moderate to strong southwest wind, 1 to 5 cm of snow expected.

TUESDAY: Overcast, freezing level around 1000 m, strong southwest wind, 1 to 5 cm of snow expected.

WEDNESDAY: Overcast, freezing level rising to about 1300 m, strong southwest wind, 1 to 5 cm of snow during the day with another 5 to 10 cm Wednesday night.

THURSDAY: Overcast, freezing level holding around 1300 m, strong southwest wind, 5 to 10 cm of snow.

On Sunday human triggered avalanches to size 2 were failing on the February 19th surface hoar, crowns were 10 to 60 cm in depth.

On Saturday storm slabs resting on surface hoar failed naturally and were sensitive to skier triggering producing slabs up to 60 cm in depth. These slabs seem to be more sensitive at and below treeline which is the reverse of how we normally think about avalanche hazard.

Some very large and destructive avalanches have been sporadically running on deeply buried weak layers near the bottom of the snowpack, predominantly on north through east aspects in the alpine. Last Tuesday, a natural size 2.5 was observed. It is suspected to have started as a wind slab in a thin rocky area before stepping down. Last Monday, two deep persistent slab avalanches size 2-3 were triggered from thin snowpack areas by very large loads pushed by snowcats. 

In most of the region 10-15 cm of recent snow has been redistributed by strong wind, the alpine is starting to look pretty wind hammered as evidenced by this MIN submission. Snow totals are deeper in the far north of the region where there is 30 to 60 cm of recent storm snow. All the new snow rests on surface hoar in sheltered locations and a sun crust on solar aspects. The surface hoar may be very sensitive to human triggering at lower elevations which is a bit different setup than we're used to.

There are few different persistent weak layers (PWL's) we're watching in the mid and lower snowpack. A patchy layer of small surface hoar crystals and a sun crust both from early February are now 30-80 cm deep. A couple of weak layers that formed in January are buried in proximity to one another 80-140 cm below the surface and continue to give hard results in snowpack tests. Below that, an early season crust lurks at the base of the snowpack. Some large avalanches have been triggered on these layers, usually during periods of rapid loading by new snow or wind and by large loads or from thin, rocky areas.

• Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
• Be aware of the potential for larger than expected storm slabs due to the presence of buried surface hoar.
• Storm slabs in motion may step down to deeply buried weak layers resulting in very large avalanches.
• The trees are not the safe-haven they normally are at this time. Terrain at treeline is primed for human triggered avalanches.