Avalanche forecast

South Coast

Apr 8 – 9, 2014Avalanche Canada
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Avalanche danger

Thu
Fri
Alpine
3 · Considerable
Treeline
3 · Considerable
Below
2 · Moderate
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Highlights

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Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible - Likely
    Size
    1–4
    Strong SW winds have set up isolated wind slab problems on leeward slopes, behind ridge crests and mid slope features like ribs/rock outcroppings. Sagging cornices may become weak with warming and solar radiation.

  • Loose Wet

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely - Very Likely
    Size
    1–3
    With warmer temperatures, limited overnight re-freeze and sunny periods on Wednesday, loose wet avalanches are likely.

  • Deep Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Unlikely - Possible
    Size
    3–7
    Three buried weak layers exist in the snowpack. Deep releases have become rare; however, the weak layers could be activated by cornice fall, a surface avalanche in motion, or intense loading from wind.

Confidence

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

Weather Forecast

An upper level ridge will keep the region fairly dry with a mix of sun and cloud through the forecast period. Wednesday/ Thursday: Cloudy with sunny periods and isolated flurries. Ridgetop winds light-moderate from the west. Freezing levels near 1300 m. Friday: Mainly cloudy with isolated flurries. Ridgetop winds light from the SW. Freezing levels rising to 1900 m.

Avalanche Summary

No new observations have been reported. On Sunday, small loose dry avalanches were seen from steep rocky terrain features. Loose wet avalanches were also seen on solar aspects. Natural avalanche activity may spike with solar radiation on Wednesday. Large, weak sagging cornices threaten slopes below if they fail.

Snowpack Summary

Up to 20 cm of new snow sits above a mix of surface hoar, facets and melt freeze crusts. The new snow seems to have a poor bond to old surfaces and isolated wind slabs likely exist. Surface snow has become moist on most aspects with the warmer temperatures and rising freezing levels. Large sagging cornices threaten slopes and could fail when the sun comes out. Snowpack tests have been producing hard resistant planar shears on the late March crust down 30-50 cm and the upper snowpack has strengthened.A couple persistent weak layers exist deeper in the snowpack. The March melt-freeze crust/surface hoar is reported to be down 60 - 100cm. The February crust/facet/surface hoar layer is now deeply buried down 150 - 250cm. These layers are mostly inactive at this time, but could re-awaken with extended warming, solar influence and large triggers like cornice fall.

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