Avalanche Forecast
North Columbia
A highly complex snowpack is being loaded by new snow and strong winds. Three weak layers are reactive to natural and human triggers. 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
- If triggered, the storm/wind slabs may step down to deeper layers, resulting in large avalanches.
- Avoid exposure to terrain traps where the consequence of a small avalanche could be serious.
- Be very cautious as you transition into wind affected terrain, wind slabs may be deep and touchy.
Avalanche Problem 2: Persistent Slabs
What Elevation?
Which Slopes?
Chances of Avalanches?
Expected Size?
Three persistent weak layers are lurking in our snowpack, which remain capable of producing very large and destructive avalanches. Keep the terrain choices reined in as the snowpack adjusts to the new load.
Travel and Terrain Advice
- Avoid open slopes and convex rolls where buried surface hoar may be preserved.
- Good day to make conservative terrain choices and watch for clues of instability.
- Numerous large avalanches have run on these layers in well supported, treed terrain.
Avalanche Summary
On Saturday, wind slabs and storm slabs were noted on northerly aspects at treeline and in the alpine, likely releasing on the mid-January weak layer. Small loose dry avalanches was also noted in steep terrain.
On Friday, there were several reports of small to large (size 1 to 3) storm slab, wind slab, and persistent slab avalanches, triggered naturally and by skiers and snowmobilers. Similar avalanches were reported on Wednesday and Thursday. These avalanches have been releasing on all three persistent weak layers described in the Snowpack Discussion.
Snowpack Summary
The current snowpack is complex, we now have three active weak layers that we are monitoring.
40-60 cm of storm snow and new forecasted snow for Sunday sits on a newly formed crust and/or surface hoar layer (mid-January). The crust is reportedly widespread, except for possibly at high elevations on north aspects. The mid-January surface hoar is 5 to 20 mm in size and was reported up to 2100 m and possibly higher. The recent snow fell with strong southwesterly winds, producing wind slabs in lee features. Deeper in the snowpack, the early-January persistent weak layer is 50 to 90 cm below the surface. It is composed of surface hoar on sheltered slopes as well as sun crust on steep solar aspects and is found at all elevation bands. Snowpack tests show sudden fracture characters with moderate loads and high propagation potential, and signs of instability such as whumpfs and cracking. Another weak layer buried mid-December consisting of a facet/surface hoar/crust combination is buried 90 to 150 cm deep. It is most problematic at and below tree line.
A rain crust buried in November is 100 to 200 cm deep and is likely dormant for the time being.
Weather Forecast
MONDAY: Mostly cloudy with intermittent snowfall, accumulation 5-10 cm, moderate southwesterly winds, alpine temperature near -10 C, freezing level near 800 m.
TUESDAY: Mostly cloudy with intermittent snowfall, accumulation 1-3 cm, light to moderate southerly winds, alpine temperature near -10 C, freezing level near 600 m.
WEDNESDAY: Mostly cloudy with intermittent snowfall, accumulation 5-10 cm, light to moderate southerly winds, alpine temperature -6 C, freezing level near 700 m.
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Around 60 cm of new snow has formed a slab that sits on a weak layer composed of feathery surface hoar and/or a crust. Expect the slab to be deeper in lee features due to strong south winds. The slab is sensitive to both natural and human triggers.