Get in, get after it, and get out. Conditions are approaching ideal for tackling bigger objectives, as long as you're savvy about exiting avalanche terrain before the heat of the day.
Weather Forecast
Thursday night: Clear. Light northeast winds.Friday: Mainly sunny with a mix of cloud in the south of the region. Light variable winds. Alpine high temperatures around -2 with freezing levels to 2000 metres.Saturday: A mix of sun and cloud with cloud increasing over the day. Light northwest winds shifting southwest. Alpine high temperatures around 0 with freezing levels to 2100 metres.Sunday: Mainly cloudy with isolated flurries bringing a trace of new snow. Light southwest winds. Alpine high temperatures around -1 with freezing levels to 2000 metres.Overnight freezing levels will remain elevated during this period, dropping briefly each night to between 1000 to 1500 metres.
Avalanche Summary
No new avalanches were reported in the Purcells over the past couple of days, but reports from neighbouring regions have shown the snow from Tuesday's storm reacting to skier traffic, ski cutting, and explosives control with 10-25 cm-deep slabs propagating easily over previous surface crusts. All aspects were represented in reports, with thicker wind-loaded slabs more prominent on north to east aspects and wet slabs observed on sun-exposed south to west aspects. Similar conditions were likely to exist in areas of the Purcells that received more than a skiff of new snow from Tuesday's storm. Looking forward, expect continuing warm, sunny weather to ramp up loose wet avalanche problems with each day's warming cycle.
Snowpack Summary
Variable new snow amounts of about 5 to 25 cm from a storm earlier in the week buried a surface of melt-freeze crust in most areas above 1500 metres. Below this elevation it buried variably moist or crusty surfaces. Precipitation fell as rain below about 1100 metres.The snowpack below about 1500 metres has been disappearing rapidly under the influence of sustained above freezing temperatures, strong sunshine, and rain. The chance of loose wet avalanches increases each day as these factors break down surface crusts and bring snow to its melting point.The mid snowpack is generally consolidated and strong, but exceptions may exist on north aspects above 2000 m, where a gradually strengthening layer of faceted grains buried 40 to 60 cm deep may still be preserved below an overlying slab of old and hard wind-affected snow.The base of the snowpack is composed of weak faceted snow which may coexist with a melt-freeze crust. Only one very large persistent slab was reported to have failed at this layer during last week's warming event.
Problems
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.
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.