Avalanche Forecast

FRIDAY NIGHT: Mostly cloudy, light to moderate wind from the west, treeline low temperatures around -6 C and freezing level dropping below 1000 m.

SATURDAY: Mostly sunny, moderate wind from the northwest. Warming temperatures with a possible inversion producing above freezing temperatures between 1500 and 2200 m and cooler temperatures in the valleys.

SUNDAY: Warming pattern continues with poor overnight recovery and above freezing temperatures overnight at 1500-2200 m. Increasing clouds, light wind from the west or northwest, warming throughout the day except near treeline and low alpine elevations where it stayed warm overnight.

MONDAY: Mix of sun and cloud. Decreasing moderate to light northwest wind, temperatures dropping to -5, and freezing level dropping to valley bottom.

The snowpack is quite complex right now recently producing impressive avalanche activity - events of the past week are relevant to the upcoming WARM weekend. This week we saw numerous very large (size 2.5-3.5) deep persistent slab avalanches occurring in both the Selkirks and Monashees. These avalanches failed on the early December facet/crust layer, typically 100-150 cm deep. One notable pattern is that many of these avalanches released at relatively low elevations (1700 to 2000 m) in open clearings, burns, and slide paths. In many cases, they were triggered by smaller avalanches starting at higher elevations.

There were also numerous reports of size 1-3 storm and wind slab avalanches reactive to human triggering and failing naturally. These smaller avalanches could step down to produce large avalanches in very rideable terrain.

20-40 cm recent storm snow is settling fast, wind affected in areas and has a thin surface crust on steep solar slopes. The new snow covered a layer of surface hoar or crust and is not expected to bond well in the short term. 

The top 70 to 100 cm of snow of the snowpack is generally with a variety of little layers that may or may not be a problem. Along with recent wind effect, upper snowpack layers include little surface hoar, thin crusts, and maybe even soft facets from early January. While none of these upper layers are necessarily going to remain a long-lasting problem, there is a fair bit of uncertainty about their spatial distribution and whether they will be reactive with the upcoming warming temperatures.

The primary weak layer that remains a widespread concern across the Columbias is a 100-200 cm deep crust/facet layer that formed in early December. There has been regular avalanche activity on this layer at all elevations for over a month, and we expect to see avalanche activity continue on this layer.

• It's critical to stay disciplined and choose only well supported, low consequence lines.
• Back off slopes as the surface becomes moist or wet with rising temperatures.
• Avoid thin areas like rock outcroppings where you're most likely to trigger avalanches failing on deep weak layers.
• The trees are not the safe-haven they normally are. Terrain at and below treeline is capable of producing large destructive avalanches.
• Cornice failures could trigger very large and destructive avalanches.