Limited field observations mean that this forecast should be used as your initial assessment before gathering additional information in the field.
Confidence
Low - Due to the number of field observations
Weather Forecast
Friday night: Cloudy with clear periods. No new snow.Saturday: A mix of sun and cloud. Light northwest winds. Alpine high temperatures around -7.Sunday: Mainly sunny. Light to moderate southwest winds. Alpine high temperatures around -4.Monday: A mix of sun and cloud. Strong southwest winds. Alpine high temperatures increasing to around 0 as freezing levels rise to 2500 metres.
Avalanche Summary
No new avalanches have been reported in the region. A Mountain Information Network post from Monday details a large (size 2) skier-triggered wind slab in a steeper wind-loaded feature in the alpine in the Mause Creek area in the west of the region. The slab had a depth of 25-40 cm and featured a 50 m wide crown fracture line.
Snowpack Summary
Light snowfall over Thursday buried a widespread layer of weak, feathery surface hoar crystals with about 5-10 cm of new snow. Below the surface hoar, the new snow has also buried pockets of recently reactive wind slab in wind-exposed terrain at treeline and above. This wind-affected layer sits above a complex of late-October and early-November melt-freeze crusts and facets found at the base of the snowpack at treeline and above. Snowpack depths taper quickly as elevation decreases and snow depths below treeline generally remain below threshold depth for avalanching.
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.