Be extra cautious around south slopes: they're weak, wind-loaded, and getting hit by the sun.
Confidence
Moderate - Due to the number of field observations
Weather Forecast
TUESDAY: A mix of sun and cloud, light to moderate northeast winds, alpine temperatures around -20.WEDNESDAY: Cloudy with sunny periods, light to moderate north winds, alpine temperatures around -16.THURSDAY: Cloudy with isolated flurries, light west winds, alpine temperatures around -14.
Avalanche Summary
On Sunday, several natural wind slabs were observed on all aspects and elevations during the peak of the winds. A skier also remote triggered a 70 cm deep wind slab on southwest-facing slope at treeline. Expect wind slabs to remain reactive to human triggers this week, especially on sun-exposed slopes. Also be aware that wind-loading and solar radiation may also make the persistent slab over the mid-December interface reactive in thin snowpack areas.
Snowpack Summary
Strong winds on Sunday had an extensive effect in exposed terrain at all elevations. Expect scouring, hard wind slabs, and thicker reactive wind slabs in unusual places as the winds shifted from west to northeast. Sunny weather is likely making the wind slabs extra touchy on south-facing slopes. The mid-December facet/surface hoar interface can be found buried 50-100 cm deep. The interface has been showing signs of gaining strength in thick snowpack areas, but remains a concern in thin snowpack areas throughout the region. The lower snowpack is well bonded and features a thick rain crust near the ground.
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.