Avalanche forecast

Purcells

Apr 6 – 7, 2014Avalanche Canada
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Avalanche danger

Tue
Wed
Alpine
3 · Considerable
Treeline
3 · Considerable
Below
3 · Considerable
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Highlights

The heat is on! Avalanche hazard will likely increase throughout the day, be sure your plans allow for a safe retreat from the mountains. Check out the Forecasters Blog for more info on dealing with sultry temps.

Avalanche problems

  • Loose Wet

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely - Very Likely
    Size
    1–3
    Loose wet avalanches and cornice fall will likely be a problem on all aspects after noon. This kind of activity heralds increasing likelihood of very large natural avalanches

  • Deep Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible - Likely
    Size
    4–8
    The big warm up has the potential to wake up deeply buried weak layers in the snowpack that have been dormant recently. If these monsters begin to stir, the results will be catastrophic.

Confidence

Fair - Timing or intensity of solar radiation is uncertain on Monday

Weather Forecast

Synopsis: After agonizing over weather products all morning, I'm convinced that freezing levels will exceed 2500m by Monday afternoon, and likely stay there until Wednesday morning. There's been a lot of talk about when the big warm up would finally happen, and it looks like well be staring down the barrel of it for the next 48 hours.Monday: Freezing Level: 1500m rising to 2200m - 2600m; Precipitation: Nil; Wind: Treeline: Light, SW | Ridgetop: Moderate, SWMonday Night: Freezing Level: 2500mTuesday: Freezing Level: 2400m - 2600m; Precipitation: Trace; Wind: Treeline: Light, SW | Ridgetop: Strong, SWTuesday Night: Freezing Level: 2500m lowering to 1500mWednesday: Freezing Level: 1500m - 2000m; Precipitation: 4:8mm - 4:15cm; Wind: Treeline: Moderate, NW | Ridgetop: Strong, NW

Avalanche Summary

No new avalanche activity was reported on Saturday.

Snowpack Summary

Recent warm temperatures have resulted in good settlement and bonding of the storm snow from last week, but you may find the odd skier triggerable wind slab on north through east facing aspects at and above treeline.Three persistent weak layers exist in the highly variable snowpack of the Columbias:The mid-March sun crust/surface hoar layer down 50-80cm still has potential for human-triggering in isolated areas. The early-March crust/facet/surface hoar layer down around 80-120cm has become less susceptible to human triggering, but still has the capacity to produce large avalanches.The mid-February crust/facet/surface hoar combo is typically down 60 - 120cm. Direct triggering of this layer has become unlikely, however, cornice fall, a smaller avalanche in motion or prolonged warming may wake this layer up, which would result in very large and destructive avalanches.Weak basal facets exist in many areas, but triggering is unlikely.

Regions covered