Confidence
Fair - Timing, track, or intensity of incoming weather is uncertain on Thursday
Weather Forecast
As the cold front sweeps through the interior Wednesday afternoon we'll see cooling temperatures and moderate precipitation amounts. Wednesday Night: Snow amounts up to 15cms. Ridgetop winds 40-50km/hr from the SW. Alpine temperatures near -4. Freezing levels down to 700m. Thursday: Snow amounts up to 10cms in the Western parts of the region, with up to 5cms in the East. Freezing levels around 700m. Ridgetop winds 40-50km/hr from the SW, switching to 30km/hr from the NW. Friday/Saturday: Snow amounts near 5cms. A ridge of high pressure builds bringing cooling, and dryer conditions into Saturday.
Avalanche Summary
Reports from the Eastern part of the region saw numerous natural avalanches up to size 2.5 , on North aspects @2000m. Many of the recent avalanches have occurred due to large triggers (cornice fall, explosive testing). On Monday there was a size 2 sled triggered avalanche that occurred west of Revelstoke on a South aspect near 1800m. No injuries reported. The mid-December persistent weak layer is buried down 80-120cms and is still a layer of concern. Avalanches that are failing on this layer are large-very large (sz 2-3.5). As the natural activity has somewhat tapered off, the sensitivity to skier, or sledder triggers are likely. Remote triggering (setting off avalanches from afar, with wide fractures) continues to be reported. I would also be suspicious of low angle terrain in the trees. It seems to be catching people by surprise.
Snowpack Summary
New snow up to 10cms has fallen over the region. This blankets all elevations and buries a new surface hoar layer that formed over the New Year. Reports indicate that the SH crystals range in size up to 10mm. The previous storm snow that fell over Christmas has been blown around by steady SW winds and has formed wind slabs. Wind slabs are widespread and found in exposed alpine and treeline locations. Below the surface 80-120cms lurks a surface hoar/facet/crust interface (persistent weak layer) from mid-December. Testing on this layer has shown moderate to hard results with sudden planer characteristics. This weak layer has been very reactive; producing large, destructive avalanches. It still remains a layer of concern and should continue to be on your radar. Below this layer sits a strong mid pack.
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.
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.