Regions
Northwest Coastal.
Confidence
Fair - Track of incoming weather is uncertain
Weather Forecast
The region is firmly in the grips of an Arctic Air mass. It looks like this pattern will persist through at least Thursday. Tomorrow looks very similar to today. Brutally cold temperatures: At 1500 m expect a high of -24 and low of -31. Winds will be blowing at moderate to strong values out of the E, NE at all elevations. Bundle up!
Avalanche Summary
Several natural slab avalanches to size 2 were reported on S through SW facing slopes on Monday.
Snowpack Summary
Outflow winds have redistributed the low density snow from the last storm into widespread hard & soft slabs that can be found in the alpine and at treeline. In wind sheltered areas the storm snow has been bonding quite well to the old snow surface, but it's getting pretty tough to find wind sheltered areas with the recent onslaught of brutally cold arctic winds. A thin wind slab is being reported in wind exposed areas below treeline as well.This is a very large region, and it should be noted that some areas are not seeing any wind effect at all.Snowpack depths vary from 3.5 to 5 m across the region. In this part of the province, the mid-December surface hoar/facet combo layer is inactive as it's now 2.5 m below the snow surface. For the most part, avalanche concerns are limited to storm snow instabilities.
Problems
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.
Loose Dry
Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.