Regions
Northwest Inland.
Confidence
Poor - Timing, track, or intensity of incoming weather is uncertain
Weather Forecast
Synopsis: Light precipitation until Friday, when a Pineapple Express to the south of the region will spill some moisture over into this region.Wednesday: Mostly flurries, but light snowfall (around 5cm) in higher snow areas in the west. Treeline temperature around -5C. Winds SW around 30 km/h.Thursday: Light snowfall. Freezing level rising to around 1000 m in the afternoon. Winds southwest 50 km/h becoming 80 km/h in the afternoon/evening.Friday: Moderate snowfall. Strong to extreme southwest winds, freezing level up to 1300 m.
Avalanche Summary
There were reports of natural avalanches up to size 2.5 on north facing slopes during the weekend following loading from new snow and wind. Slope testing on Monday resulted in a few size 1 slabs in steep wind-loaded features.
Snowpack Summary
A new sun crust has formed on steeper solar aspects that may be buried by light snow. In shady areas there is 40-60 cm of well settled storm snow. Strong southwest winds formed touchy wind slabs in exposed terrain in lee of ridges, in gullies, and behind terrain features. There are a variety of old interfaces now down 60 - 100cm which include facets, crusts and isolated pockets of surface hoar. Recent observations indicate that these weaknesses have bonded fairly well now, but I still suggest digging and testing the snowpack to confirm.A strong mid-pack currently overlies a weak base layer of facets/depth hoar. It is worth noting that the snowpack in general is quite shallow in northern and eastern parts of the region. Triggering the basal weakness may still be possible from thin spots, rocky outcrops or under the weight of larger triggers such as cornice fall.
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.
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.