The recent snow has added load to buried weak layers and may still be reactive to human triggers. Conservative terrain selection is recommended.
30 to 60 cm of settled snow rests above a widespread layer of surface hoar that produced numerous avalanches last week. These slabs have been most sensitive to triggering at treeline.
10-20 cm of fresh snow and wind has formed storm slabs in many areas, especially at higher elevations. These slabs may be more reactive to human triggers in wind loaded areas, and in the trees, where they likely rest on a buried surface hoar layer.
Recent loading from new snow and wind has aggravated the region's deep persistent slab problem. Some very large and destructive avalanches have been sporadically failing on deeply buried weak layers, predominantly on north through east aspects in the alpine. Cornice falls are a likely trigger for these slabs.
WEDNESDAY NIGHT- Cloudy with clear periods and isolated flurries / northwest wind, 30-40 km/h / alpine low temperature near -12
THURSDAY- A mix of sun and cloud / northwest wind, 20-30 km/h / alpine high temperature near -10
FRIDAY- Sunny with cloudy periods / northeast wind, 30-60 km/h / alpine high temperature near -14
SATURDAY- Sunny / northeast wind, 40-80 km/h / alpine high temperature near -8
Fresh snow and strong winds have promoted storm slab development, especially at upper elevations. Humans may be able to trigger these slabs, especially in wind loaded areas and in the trees, where a buried surface hoar layer may make these slabs more reactive.
Last week there were reports of wind slab, persistent slab (failing on the February 19 surface hoar layer), and deep persistent slab (failing on basal facets) avalanches. This pattern highlights loading and surface avalanches from recent stormy weather straining multiple weak layers in the snowpack.
The recent storm delivered 10-20 cm of new snow to the region with strong winds. This new snow is likely sitting on a weak layer of surface hoar, and/or a crust on solar aspects. There are likely widespread storm slabs at upper elevations within the new snow.
Loading from new snow and wind has made several persistent weak layers problematic over the past week. A combination of surface hoar and sun crust layers were buried on February 19 and currently sit 30-60 cm below the surface that seem to be most sensitive to human triggering at treeline elevations.
A couple of weak layers that formed in January are buried in close proximity to one another 80-140 cm below the surface. Below that, an early season crust/facet layer lurks at the base of the snowpack.
