Regions
Northwest Inland.
Warm, sunny conditions are increasing the range of avalanche problems as well as their potential for reactivity.
Weather Forecast
Thursday: Sunny with lingering valley cloud due to an alpine temperature inversion. Light southwest winds. Freezing level to 3200 metres with alpine temperatures around +5. Cooler at lower elevations.Friday: A mix of sun and cloud with cloud increasing over the day. Moderate to strong southwest winds. Freezing level dropping to about 2000 metres as the temperature inversion breaks down. Alpine temperatures around 0.Saturday: Mainly cloudy with isolated flurries and a trace of new snow. Light to moderate southwest winds. Freezing level to about 1700 metres with alpine temperatures around -1.
Avalanche Summary
No recent avalanche activity has been reported, however stiff wind slabs now exist at treeline and in the alpine on leeward slopes and cross-loaded features. If triggered, these could step down to deeper weak layers and initiate large avalanches. The last significant avalanche observation was submitted on November 28th from Skilokis Creek. Here, a size 2.5 persistent slab was triggered from 150 m away. The possibility for further persistent slab activity will be elevated while temperatures remain unseasonably warm.
Snowpack Summary
Average snowpack depths now total 80-140 cm at treeline elevations and up to 160 cm in the alpine. (Depths of up to 210 cm have been reported from the Howsons.) Wind effect from recent strong southwest to northwest winds penetrated down into treeline elevations and resulted in fairly extensive wind slab formation. Below the wind-affected surface, approximately 30-50 cm of recent snow now overlies two crusts that were buried near the end of November. These crusts are widespread and extend into the alpine. Although recent snowpack tests have shown hard results at these crust interfaces, observations have been limited. Below these crusts, a well settled midpack overlies the late October crust near the base of the snowpack. This "crust/facet combo" is widespread and has been reactive to rider and remote triggers.
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.
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.