Watch for pockets of wind slab on steep, convex terrain.
Confidence
Poor - Due to the number of field observations
Weather Forecast
Cold, clear weather looks set to continue through the weeekend.Saturday: Dry, temperatures around -28C, light NW winds.Sunday: Dry, temperatures around -22C, strong NW winds.Monday. A few flurries, maybe 1-2 cm new snow. Temperatures around -17C. Strong NW winds.
Avalanche Summary
No recent avalanche activity to report.
Snowpack Summary
Snowpack depth varies greatly across the region, averaging 70-110cm at treeline. The southern portion of the region received substantially more new snow (up to 70cm ) compared to the northern portion (as little as 10cm). The recent storm snow is sitting on top of the late-November interface which may consist of surface hoar on sheltered/shaded slopes, a melt-freeze crust on south facing slopes, or a combination of both in isolated locations. Strong NE winds after the storm have caused reverse loading and wind slab formation on SE through W aspects in wind exposed areas. In the southern part of the region there is 40-70cm of new snow over the late-November interface which has created a persistent slab problem. Expect the reactivity of this layer to increase when we eventually get warmer temperatures and new snow.In the northern part of the region the lower/mid snowpack is fundamentally weak, composed of an early season crust (more prevalent on north aspects) and weak faceted crystals. While many areas did not receive enough new snow to create a new slab problem on top of the late-November interface, there are likely isolated areas where a persistent slab does exist.
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.
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.