Confidence
Fair - Intensity of incoming weather systems is uncertain on Thursday
Weather Forecast
Thursday: Light to locally moderate precipitation. Winds moderate west. Freezing level 1800m.Friday: Overcast with flurries. Moderate northwest winds. Freezing level 1500m.Saturday: Mix of sun and cloud. Light west wind. Freezing level 2200m.
Avalanche Summary
Recent reports are limited to solar triggered avalanches to size 2 from south facing terrain in the alpine and tree-line.
Snowpack Summary
Moist snow and/or a crust exist on all aspects and elevations except for high elevation north-facing terrain. A melt-freeze crust buried at the beginning of April can be found 40-50cm below the snow surface. This layer has been variably reactive in snowpack tests. Three persistent weak layers exist in the highly variable snowpack of the South Columbia region:-The mid-March sun crust/surface hoar layer down 50-80cm and the early-March crust/facet/surface hoar layer down around 80-120cm seem to be inactive.-The mid-February crust/facet/surface hoar combo is typically down 150 - 200cm. Direct triggering of this layer has become unlikely, however, cornice fall, a smaller avalanche in motion or prolonged warming could wake this layer up, which would result in very large and destructive avalanches.
Problems
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
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.