Recently formed wind slabs and touchy persistent weak layers are making for tricky conditions. Conservative terrain selection remains important.
Confidence
Moderate - Due to the number of field observations on Sunday
Weather Forecast
A ridge of high pressure off the coast will slowly move eastward on Monday and should be established over the interior by Tuesday. Mostly cloudy conditions are expected for Monday with sunny breaks and light scattered flurries both possible. Alpine winds are expected to be light from the northwest in the morning but may become moderate in the afternoon. Freezing levels are expected to be below valley bottom during the over periods and stay below 1000m in the afternoons. A mix of sun and cloud is expected for Tuesday with light to moderate northwest winds in the alpine. Increasing cloudiness is expected for Wednesday in advance of a weak storm system that is currently forecast to arrive on Wednesday night.
Avalanche Summary
On Saturday, no natural avalanches were observed but several size 1 skier and explosive triggered avalanche were reported. Most of the skier triggered avalanches were 15-25cm thick wind slabs on north and east aspects at 2100-2300m. Explosives triggered several loose dry avalanches on northwest aspects in the alpine. On Friday, widespread natural avalanche activity up to size 3 was reported in throughout the region. This includes both storm slabs releasing down 30-60cm and persistent slabs failing down 70-100cm on the early January surface hoar layer. The storm slabs were failing on all aspects from 2000 to 2500m while the persistent slabs were failing on a variety of aspects around 1500-1900m. One persistent slab was also reported from 2300m on a southwest aspect. A skier accidently triggered a size 2 persistent slab avalanche on an east aspect at 1600m on the early January surface hoar layer down 70-80cm. Recently formed wind slabs and a reactive persistent slab are both expected to remain sensitive to human-triggering on Monday.
Snowpack Summary
Recent storm loading brings storm slab thickness to 20-40cm and up to 50cm in wind loaded areas. The recently destructive persistent weak layer from early January is now typically down 70-110cm in most places and has recently produced some large, destructive avalanches in the region. The layer is slowly getting harder to human trigger but is still quite reactive in snowpack tests and has the potential for wide propagations. In general, the lower snowpack below this layer is well settled and strong.
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.