Sheltered areas have some good skiing and we have not seen much recent avalanche activity...but watch for wind slabs at higher elevations and stay a bit wary of the mid pack surface hoar layers at treeline in Little Yoho.
Weather Forecast
The forecast is for periods of snow starting on Monday night and continued flurries through Tuesday and Wednesday with total accumulations of up to 10 cm. Temperatures should stay in the -8 to -15 range at treeline and winds will be moderate to strong out of the West, possibly easing off on Wednesday.
Snowpack Summary
A few cm of new snow Sunday night. Wind effect in open areas at treeline and above with faceted surface snow below treeline. Three mid-pack weak layers of surface hoar and/or facets are down 100-130cm and gaining strength, but are worth keeping in mind on bigger slopes. Thin snowpack areas are facetting and weakening with the cold temperatures.
Avalanche Summary
Reports of thin wind slabs triggered by ski cutting and explosives in lee areas at the local ski resorts. No other recent avalanche observations in the Little Yoho region.
Confidence
Forecast snowfall amounts are uncertain on Wednesday
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.