Avalanche Forecast
Cariboos
The snowpack is complex. Three active weak layers remain sensitive to human triggering. The easy solution is to choose simple terrain free of overhead hazard as the snowpack adjusts.
Avalanche Problem 1: Storm Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
Travel and Terrain Advice
- Be very cautious as you transition into wind affected terrain, wind slabs may be deep and touchy.
- Carefully investigate the bond of the new snow before stepping out into more challenging terrain.
- If triggered the storm/wind slabs may step down to deeper layers resulting in large avalanches.
Avalanche Problem 2: Persistent Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
The riding conditions may be great, but we can't forget about the persistent weak layers lurking in our snowpack that remain quite capable of producing very large avalanches. Keep the terrain choices reined in as the snowpack adjusts to the new load.
Travel and Terrain Advice
- Numerous large avalanches have run on these layers in well supported, treed terrain.
- Good day to make conservative terrain choices and watch for clues of instability.
Avalanche Summary
On Thursday avalanche activity was reported as storm and persistent slabs. Storm slabs were running to size 2 on southerly and northerly aspects in the alpine and tree line. There were two persistent slab avalanches reported that were both skier triggered 80cm deep between 1100 and 1400m on north aspects. One of them was remotely triggered (from a distance) from 60m away and was a size 2.5. The other was triggered by a ski cut and was a size 1, yet still 80cm deep.
On Wednesday a small natural avalanche cycle was reported from steep ridge features. Fast and loose sluffing was also reported.
Snowpack Summary
The current snowpack is complex, we now have three active weak layers that we are monitoring.
15-35cm of storm snow now sits on a newly formed crust and/or surface hoar interface. Prior to the storm the crust was reportedly widespread; high elevation north is likely one of the few crust-free zones. The now buried surface hoar is up to 10mm in size and was reportedly present at all elevations before the storm. Looking deeper, a persistent weak layer known as the early January interface is 30 to 60 cm below the surface. It is composed of surface hoar on sheltered slopes as well as sun crust on steep solar aspects and is present at all elevation bands. Recent snowpack tests have shown sudden results with moderate loads. Additionally, yet another persistent weak layer buried mid-December consisting of a facet/surface hoar/crust combination, is buried 40 to 100 cm deep. It is most problematic at and below tree line. This interface is not thought to be present in the alpine.
A rain crust buried in November is 100 to 150 cm deep and is thought to have gone dormant for the time being.
Weather Forecast
SATURDAY: Mix of sun, cloud and isolated flurries / Light to moderate southwest wind / Alpine temperature -10 / Freezing level 1100m
SUNDAY: Flurries, accumulation 5-10cm / Moderate to strong south wind / Alpine temperature -10 / Freezing level 900m
MONDAY: Scattered flurries / Light southwest wind / Alpine temperature -12 / Freezing level 800m
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15 to 35cm sits on a combination of crust and surface hoar. Expect the slab to be deeper in wind exposed features and to be sensitive to human triggering.