Watch for winds slabs in open terrain and around ridge features. Deeper and more reactive deposits will be in lee and cross-loaded terrain.
Confidence
Moderate - Wind effect is extremely variable
Weather Forecast
TUESDAY NIGHT: Clear with cloudy periods. Alpine temperatures near -18C. Ridgetop winds 20-25 km/h from the east.WEDNESDAY: Sunny with cloudy periods. Alpine temperatures near -15C. Ridgetop winds 15-25 km/h east.THURSDAY: Mostly cloudy with scattered flurries, trace to 6 cm snow. Alpine temperatures near -10C. Ridgetop winds around 15 km/h from the east.FRIDAY: Mainly cloudy with scattered flurries, 5 cm snow. Alpine temperatures near -18C. Ridgetop winds 25-30 km/h from the east.
Avalanche Summary
On Monday, small and thin (size 1) natural wind slab avalanches were reported on west to south-south east aspects. Similar small, thin slabs were reactive to skiers on north to east-southeast aspects at treeline and above. Additionally, a machine operator on a road at 1700 m triggered a small (size 1) slab avalanche with a 40 cm crown which failed on on a layer of well preserved surface hoar between crusts.Last Saturday, numerous natural and explosives triggered storm slab avalanches to size 2-2.5 were reported. These were 50-100 cm deep running on east through north aspects in the alpine and treeline. Loose, dry snow is sloughing in steeper terrain. On Sunday, a skier triggered a size 1 storm slab avalanche on a north aspect around 2100 m.Last Thursday, before the weekend snowfall, an explosive triggered a large (size 2.5) persistent slab avalanche. The slab was about 40 cm deep and failed on a southerly aspect between 1650 and 2000 m.
Snowpack Summary
Winds are redistributing recent snowfall forming scouring ridgetops and producing wind slabs in open areas at treeline and above. The recent snow covered wind-affected surfaces in the alpine and treeline. In sheltered areas and lower elevations, the new snow is burying faceted surface snow and a patchy layer of surface hoar. Between 1600-1800 m, another weak layer of surface hoar crystals buried around Valentines Day, is now 50-80 cm below the snow surface.Two more weak layers of surface hoar may be found within the snowpack. One buried early-February, is 40-80 cm deep in shaded and sheltered areas above 1600 m. The other buried mid-January, is 100-120 cm down and is most prominent between 1600-1900 m.The remainder of the snowpack is well-settled.
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.