Snow, rain and wind combined with buried weak layers make the perfect recipe for avalanches. The upper snowpack is complex, keep it simple and use a very conservative approach to terrain selection.
Weather Forecast
A series of pacific frontal systems will bring waves of precipitation to the Interior Ranges over the forecast period. Friday will see overcast skies, precipitation amounts 5-15 mm, ridgetop winds moderate from the SW and freezing levels 1700-2000 m. Continued precipitation on Saturday with amount up to 15 mm , ridgetop winds light-moderate from the SW and freezing levels near 1800 m. Later Saturday the front will start to move east setting up a clearer, drying trend for Sunday. Freezing levels will initially drop to valley bottom overnight Saturday then rise steadily during the day with treeline temperatures near 0 degrees.
Avalanche Summary
On Wednesday, natural and skier triggered slab avalanches were reported up to size 2. Both avalanches were reportedly over steeper convex terrain features on northerly aspects above 2100 m. Widespread natural avalanche activity is expected through the weekend due to new snow, rain and strong SW winds. Avalanches failing on the the mid-February persistent interface will likely have wide propagations and be large and destructive.
Snowpack Summary
At higher elevations, new storm snow up to 20 cm sits over a plethora of surfaces including moist snow, crusts, wind affected surfaces, and/or old wind slabs. This gives us anywhere from 40-80 cm over the mid-February persistent weak interface. This interface has recently been very reactive and I don't suspect that to change during this stormy period. Strong winds have redistributed new snow into wind slabs on leeward terrain features. Lower elevations up to treeline are sporting spring-like, melt-freeze conditions. The late-January crust/surface hoar layer (over 1m deep) and the mid-January surface hoar (around 1.5m deep) have been dormant for several weeks.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.
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.