Avalanche Forecast
Cariboos
Recent storm snow has been reactive on steep slopes. The presence of buried weak layers increases the potential size of avalanches.
Avalanche Problem 1: Storm Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
Travel and Terrain Advice
- The new snow may require several days to settle and stabilize.
- If triggered the storm slabs may step down to deeper layers resulting in large avalanches.
- Stay off recent wind loaded areas until the slope has had a chance to stabilize.
Avalanche Problem 2: Persistent Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
Several troublesome layers exist in the snowpack and may be reactive to large triggers such as a cornice or storm slab release. Human triggering may also be possible in shallow or thin, rocky areas.
Travel and Terrain Advice
- Pay attention to overhead hazards like cornices which could easily trigger persistent slabs.
- Minimize exposure to overhead avalanche terrain, large avalanches may reach run out zones.
- Avoid steep convexities or areas with a thin or variable snowpack.
Avalanche Summary
On Wednesday, several avalanches were reported in recent storm snow up to size 2.5. Previously, a very large, widespread natural avalanche cycle up to size 4 was observed last week. Slopes of all aspects and elevations ran full path and reached valley floor. In some cases, mature timber was destroyed. Many of these failed on persistent weak layers mentioned in the snowpack discussion. Although natural avalanche activity on these layers has tapered-off, human triggering of very large avalanches remains a very real possibility.
Snowpack Summary
25cm of recent storm snow is settling into a slab in the upper snowpack. Wind data has been sparse, although I suspect strong winds have shifted these accumulations into deeper, reactive slabs in wind-exposed terrain. These accumulations overlie a mix of older wind slabs in exposed higher elevation terrain, a sun crust on steep solar aspects and surface hoar on sheltered slopes.
Below the snow surface, several persistent weak layers make up a troublesome snowpack. In the top 1-1.5 m of the snowpack, two surface hoar layers buried in January can be found. Expect to find at least one of these layers on all aspects and elevations.
Deeper in the snowpack (120-200 cm deep) is a facet/crust/surface hoar layer from December, most prevalent at and below treeline.
Near the base of the snowpack is a crust/facet combo, most likely to be triggered from thin spots in the alpine.
All of these layers have produced large avalanches recently. The wide distribution and ongoing reactivity of these layers suggests that avoidance through choosing simple terrain is the best strategy.
Weather Forecast
Friday: 5-10 cm new snow. Treeline temperature around -7C. Westerly ridgetop winds gusting to 50 km/h.
Saturday: 2-5 cm new snow. Treeline temperature around -12C. Light variable winds.
Sunday: Sunny but cold. Treeline temperatures around -17C. Winds light northeasterly.
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New storm slabs may be especially reactive in wind-exposed terrain, and may be slow to gain strength due to a mix of underlying weak surfaces. Watch for new wind slab development and reverse loading due to northwest winds on Thursday.