Regions
Northwest Inland.
Fresh storm slabs have formed after a stormy weekend and persistent snowpack weaknesses have yet to fully heal. Sustained strong winds will keep conditions touchy on Monday.
Weather Forecast
Monday: A mix of sun and cloud with isolated flurries and a trace of new snow. Winds moderate to strong from the northwest. Alpine temperatures of -11. Tuesday: A mix of sun and cloud. Winds light to moderate from the northeast. Alpine temperatures of -12 Wednesday: A mix of sun and cloud. Winds light from the east. Alpine temperatures of - 10.
Avalanche Summary
Stormy weather has been obscuring visibility of higher elevation avalanche terrain, but a natural cycle was at least audible and suspected to Size 3 in the Howson Range on Saturday. Warm valley temperatures also allowed a number of loose wet avalanches to be observed occurring at lower elevations on Friday. Aside from new storm slabs that have formed and become a problem in their own right, it should be noted that these slabs have introduced a new load above our deeper snowpack weaknesses, increasing their likelihood of triggering. It remains to be seen to what extent avalanche activity over Saturday and Sunday has involved these deeper persistent weaknesses, but sustained strong winds and a changing wind direction can be expected to promote instability over the short term.
Snowpack Summary
Stormy weather over Friday to Sunday morning has delivered anywhere from 30-60 cm of new snow to the region. Including snow from earlier in the week, 40-80 cm of storm snow now sits above a widespread rain crust up to about 1300 m. At treeline and above, the storm snow is settling above wind slabs that formed on lee and cross loaded features in days before the storm. Our new snow has effectively shifted this wind slab problem into a more generalized storm slab issue. Below our the storm snow forming the upper snowpack, several buried surface hoar layers can be expected roughly 50-100 cm deep. Before the storm, these layers had been yielding moderate to hard results in snowpack tests. Many areas have hard slabs in the mid snowpack above weak sugary snow near the ground. Triggering a deep persistent slab above this sugary snow will remain a low probability high consequence scenario for some time, with probability increasing as sustained strong winds redistribute loose snow and add load to specific areas of the snowpack.
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.