Regions
Northwest Coastal.
Pockets of reactive wind slab remain a concern for wind-exposed alpine and treeline areas. Watch for stiff or hollow feeling snow and shooting cracks.
Confidence
Moderate - Due to the number of field observations
Weather Forecast
THURSDAY NIGHT: Light snow. Accumulation 2 cm. Ridge wind light southeast. Temperature -20. Freezing level surface.FRIDAY: Mix of sun and cloud. Ridge wind light southeast. Temperature -18. Freezing level surface.SATURDAY: Mostly sunny. Ridge wind moderate northwest. Temperature -18. Freezing level surface.SUNDAY: Mostly sunny. Ridge wind light northwest. Temperature -15. Freezing level surface.
Avalanche Summary
No recent avalanches have been reported. A skier remotely triggered a large wind slab (size 2) near the Shames area on Sunday. The avalanche was triggered on a steep south-facing rocky ridgetop at 1400 m.
Snowpack Summary
Strong outflow winds have affected the surface snow over the past week, scouring some slopes down to an old crust and forming hard deposits in many other areas. Sheltered areas may still have 30 cm of powder from previous storms, but winds have come from a variety of directions and affected much of the terrain. Wind slabs rest on a variety of old surfaces including a thick melt-freeze crust that formed in mid-December. In some sheltered locations, soft feathery surface hoar crystals may sit above this crust.The snowpack is reported to be generally strong below this crust, with the possible exception of areas around Stewart and northern parts of the region where the late-October crust can be found deep in the snowpack. Weak sugary snow may exist around the crust and could be triggered from shallow snowpack areas.
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.