Preemptive avalanche control is planned for Mt. Stephen, Mt. Field and the Simpson Slide Paths. No activities in these areas tomorrow. Expect a major system with significant snowfall starting late tomorrow.
Weather Forecast
A major system is heading for the forecast region starting late tomorrow. The models have varying data but upwards of 40cm is expected throughout Thursday and Friday. The system is accompanied by warm temperatures. Surprisingly, wind does not appear to be increasing when the front tracks through the forecast region, but this could easily change.
Snowpack Summary
Wind effect exists in the alpine and at treeline. Below treeline, the surface is faceted powder. This overlies the Dec. 10th layer of facets and depth hoar which is down 60-100 cm. In thin snowpack areas, the Dec. 10th layer is mixed in with the basal facets and October crust. In thicker areas, it is a distinct layer, with a stronger snowpack below
Avalanche Summary
No new avalanches observed or reported today however potential for human triggering remains.
Confidence
Intensity of incoming weather systems is uncertain on Thursday
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.