Strong wind will continue blowing. Expect wind-loaded pockets around ridge crest in upper elevations.
Exposed slopes at higher elevations will continue to see effects from the incoming winds. Lingering and new wind slabs could remain reactive in open areas. While these slabs may be thin, they could be poorly bonded to the underlying snow, so be extra cautious in lee terrain and convex rolls.
A persistent slab problem formed by a crust down 100-270 cm has created a low likelihood, high consequence scenario that is difficult to forecast. There has been an increase of avalanche reports on this deep layer recently. This problem is likely to be triggered on steep, rocky slopes with a shallow or thin-to-thick snowpack. The same feature or path can slide repeatedly when the persistent weak layer is reloaded with new snow.
SUNDAY NIGHT: Partially cloudy, strong west wind, treeline low around -5 C, freezing level around 1000 m.
MONDAY: Snow late afternoon 5 cm, treeline high around -3 C, strong southwest wind, freezing level around 1500 m.
TUESDAY: Snow, 5 cm, light variable winds, treeline high around -10 C, freezing level returning to valley bottom.
WEDNESDAY: Clearing, light southwest winds, treeline high around -12 C, freezing level returning to valley bottom.
No new avalanches were observed nor reported in the last 24 hours.
Thursday, three very large avalanches were reported from this region. The avalanches appear to have failed on the early December crust and showed wide propagation. They occurred on southwest to southeast aspects and were naturally triggered in response to rising temperatures and solar radiation.These avalanches follow a previous sporadic pattern of very large avalanches that have been reported from this region and neighbouring regions over the last couple of weeks.
Fresh dry snow can still remain at upper elevation but will be most likely wind affected. Around 2000 m and below, a crust is now capping the dense 15 cm of snow which has settled significantly with the past mild temperatures. The crust varies from thin/breakable to thick/supportive, according to the aspects and elevation. Under it, the snowpack consists of a variety of old surfaces, including soft snow in sheltered areas and wind slabs in exposed and open areas, which formed over the past few days.
The most notable layer of concern in the snowpack is a crust that was formed in early December and is now down 100-270 cm. This layer appeared to have "waken up" in response to warm temperatures and solar radiation on Thursday Jan 13, when at least three very large avalanches were reported on this layer. This layer has created a low likelihood, high consequence scenario which is best managed through conservative terrain choices and disciplined backcountry travel techniques.
