Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Regions
Northwest Coastal.
The avalanche danger may be higher in the north of the region where very large, full depth avalanches remain a concern
Confidence
High - The weather pattern is stable
Weather Forecast
Saturday: Sunny / Moderate east wind / Alpine temperature -16Sunday: Sunny / Moderate northeast wind / Alpine temperature -17Monday: Mix of sun and cloud / Light east wind / Alpine temperature -16More details can be found on the Mountain Weather Forecast.
Avalanche Summary
There are no recent reports of natural avalanche activity from the past few days in the southern and middle portions of the region. However, in the northern most parts of the region near Bell2 or Ningunsaw there are still reports of skier triggered avalanches stepping down to basal facets in the alpine and tree line.
Snowpack Summary
The snow from last week has been long redistributed by continuous strong winds to create widespread wind effect at upper elevations. At lower elevations, precipitation fell as rain and a surface (or near-surface) crust may now be found below about 1000m. Below the recent storm snow you'll likely find a couple of buried surface hoar layers from January 18th and January 23rd. These surface hoar layers continue to produce easy to hard sudden shears in snowpack tests, and should be approached with caution, especially in sheltered tree line terrain. The snowpack below this is generally strong and well settled. The exceptions are areas around Bear Pass and Ningunsaw where basal facets remain an ongoing concern.
Problems
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.