Regions
Northwest Coastal.
Sustained winds have produced new wind slabs in lee features. Increasing freezing levels and sunny skies are intensely warming the snowpack. The best riding will be in areas sheltered from the wind effect and sun, without any overhead exposure.
Confidence
Moderate - Timing or intensity of solar radiation is uncertain
Weather Forecast
MONDAY: Partly cloudy, moderate southerly winds, alpine temperature 2 C, freezing level 2000 m.TUESDAY: Mostly sunny, light to moderate southeasterly winds, alpine temperature 4 C, freezing level 2200 m.WEDNESDAY: Cloudy with light snowfall, accumulation 5 cm, light southerly winds, alpine temperature 0 C, freezing level 1400 m.
Avalanche Summary
Wind slabs were reactive to skier traffic and natural activity on Saturday. Numerous size 1 to 2 avalanches were reported, generally 10 to 30 cm deep and at treeline and alpine elevations on northerly aspects. Many of these avalanches travelled fast and far when sitting on weak surface hoar. Loose snow was also noted in steep terrain features.
Snowpack Summary
Sustained southerly winds have redistributed the 20 cm of new snow and produced wind slabs in lee features. This overlies a sun crust on solar aspects and 5 to 20 mm surface hoar on sheltered, shady aspects at all elevation bands. Expect to find a melt-freeze crust early mornings and moist snow with warming below around 1500 m.Beneath this, expect layers of crusts, facets, and isolated surface hoar buried 50 to 100 cm below the surface from mid- and late-February. A surface hoar and crust layer from January is buried around 150 to 200 cm.Near the bottom of the snowpack, sugary facets exist in colder and dryer parts of the region, such as the far north.
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 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.