Weather Forecast
The region will continue to see unsettled weather conditions overnight Monday, bringing light snow (5-10 cm) with moderate Northerly winds. Freezing levels will fall to valley bottom. Tuesday: Flurries in the morning. Freezing levels remain valley bottom. Wednesday: Mix of sun and clouds. Ridgetop winds moderate from the NW. Treeline temperatures near -8. Freezing levels at valley bottom, rising 800-1000 m in the afternoon. Thursday: Dry, sunny conditions with rising freezing levels 15-2000 m. Ridgetop winds light from the SW.
Avalanche Summary
A natural avalanche cycle began on Saturday in response to snow, wind and warming. Operators are reporting numerous size 1-3.5 natural avalanches, starting in the alpine on all aspects. Skier-triggered slabs were also reported in the size 1-2 range, failing on storm snow weaknesses. Previously this week, many avalanches were triggered remotely (from several hundred metres away) and accidentally by skiers and machinery. These avalanches failed on upper snowpack persistent and storm snow weaknesses, on a variety of aspects and elevations.
Snowpack Summary
Over the weekend, 50-70 cm storm snow fell. Strong winds from the SW and fluctuating temperatures are a perfect recipe for storm slab, and wind slab instabilities. This new snow has buried variable old surfaces (surface hoar, facets, and crusts) that formed mid-February. These persistent weak layers have remained touchy all week and are a key concern at all elevations. Storm slabs, wind slabs, sluffs, and riders could trigger these deeper layers, creating avalanches which are larger than you expect. Large cornices have formed and loom as potential triggers for deep avalanches.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.
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.