North Columbia

Substantial snowfall is forecasted for most of the region, which will rapidly load several buried weak layers. Travel in avalanche terrain is not recommended where local accumulation reaches 30 cm, as widespread avalanche activity is expected.

Moderate - Timing, track, or intensity of incoming weather system is uncertain

TUESDAY NIGHT: Cloudy with snowfall, accumulation 10 to 20 cm, moderate westerly winds, alpine temperature near  -8 C, freezing level below valley bottom.WEDNESDAY: Cloudy with snowfall, accumulation 15 to 30 cm, moderate to strong westerly winds, alpine temperature near -4 C, freezing level near 1400 m in the south of the region and below valley bottom in the north of the region.THURSDAY: Cloudy with snowfall, accumulation 15 to 30 cm, moderate westerly winds, alpine temperature near -8 C, freezing level below valley bottom.FRIDAY: Partly cloudy with possible valley cloud, light to moderate northwesterly winds, alpine temperature near -14 C, freezing level below valley bottom.

Many slab avalanches were reported in the region on Monday, including storm/wind slabs and persistent slabs.  The storm and wind slabs were generally 20 to 30 cm deep, but as deep as over 100 cm in wind-loaded features.  They were on all aspects, generally at treeline and alpine elevations, and triggered naturally, by explosives, and skiers.  The persistent slab avalanches released on all of the layers discussed in the section below, they were between 100 and 400 cm deep, on all aspects, and triggered naturally, by explosives, and skiers.  Similar avalanches were reported between Friday and Sunday, showing a steady trend of avalanche activity.Looking forward, dangerous snowpack conditions will persist in the region, particularly with forecasted snowfall on Wednesday.  This trend will likely continue until a more stable weather pattern governs and we see a decrease in avalanche observations. All of our buried weak layers (described below) continue to produce large, destructive avalanches from natural and human triggers. Recent storm slabs and wind slabs have the potential to step down to deeper weak layers, which could produce large, destructive avalanches.

Up to 50 cm of snow could accumulate in the region on Wednesday.  This overlies 100-200 cm of storm snow from the past two weeks that has formed widespread storm slabs as well as wind slabs in lee features, which sit over an unstable snowpack.  There are four active weak layers that we are monitoring:1) 80 to 150 cm of snow sits on the crust and/or surface hoar layer from mid-January. The crust is reportedly widespread, except for possibly high elevation north aspects. The surface hoar is 5 to 20 mm in size and was reported up to tree line elevations and possibly higher.2) The early-January persistent weak layer is 120 to 170 cm below the surface. It is composed of surface hoar on sheltered slopes as well as sun crust on steep solar aspects and is found at all elevation bands.3) Another weak layer buried mid-December consists of a facet/surface hoar/crust combination, which is buried 200 cm or more below the surface. It is most problematic at and below tree line.4) A crust/facet layer from late November is yet another failure plane responsible for recent very large avalanches.