Regions
Northwest Coastal.
Strong to extreme wind and new snowfall are expected to drive a natural avalanche cycle. We cannot trust the weak layers formed during the drought with this kind of loading, so rein the terrain choices way in and steer clear of overhead hazard.
Confidence
Moderate - Timing, track, or intensity of incoming weather system is uncertain on Saturday
Weather Forecast
A severe wind event is expected to impact the region Saturday before a significant warm up begins on Sunday. Next week looks to be very warm with the freezing level approaching 3000 m by Tuesday. Unfortunately, very little overnight re-freeze is expected during the warm spell.FRIDAY NIGHT: Freezing level around 600 m, moderate to strong southwest wind, 2 to 8 cm of snow.SATURDAY: Overcast, freezing level rising to 1000 m in the afternoon, strong to extreme southwest wind, 5 to 15 cm of snow. SUNDAY: Broken cloud cover, moderate to strong south/southwest wind, freezing level approaching 2000 m, a few mm of precipitation possible.MONDAY: Scattered cloud cover, moderate to strong south/southwest wind, freezing level approaching 2500 m, no significant precipitation expected.
Avalanche Summary
Recent avalanches can be divided into two classes -- light triggers and large triggers. For light triggers there are reports of wind and storm slabs up to size 2.5 on northerly aspects in northern areas . Throughout the region there were reports of a solar triggered cycle up to size 2 on solar aspects. Closer to Terrace there was a report of small soft slab triggered by a skier, a wind slab cycle up to size 1.5 (due to some strong southerly winds), and some loose dry avalanches, possibly as large as size 2. Most recent avalanche activity was a result of larger triggers, namely explosives. Explosive tests and control resulted in mostly size 2 avalanches but in some inland areas in the east side of the region avalanches up to size 3.5 were triggered. Strong to extreme southwest wind Saturday combined with new storm snow is likely to initiate a natural avalanche cycle.
Snowpack Summary
Continued snowfall is adding to the 40-60 cm of previous storm snow. The recent snow is settling but is covering a wide variety of old snow surfaces: crusts on solar aspects, facets up high, and surface hoar in sheltered locations. Not much further below this storm snow interface is a second weak layer buried on February 19 made up of weak facets and surface hoar crystals. Recent avalanche activity was more or less equally split between these two layers.The lower snowpack is generally strong.
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.
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.