Avalanche forecast

South Coast

Jan 23 – 24, 2015Avalanche Canada
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Avalanche danger

Sun
Mon
Alpine
4 · High
Treeline
3 · Considerable
Below
3 · Considerable

Highlights

The wet, warm, and windy storm will result in High avalanche danger.

Avalanche problems

  • Storm Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely
    Size
    1–4
    New storm slabs are expected to develop due to forecast snow and strong winds.
  • Loose Wet

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Likely
    Size
    1–3
    Forecast warm temperatures and high freezing levels may result in loose wet avalanches starting in steep terrain.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Warm, wet, and windy overnight as another 10-15 mm of precipitation moves into the region. The freezing level is expected to be about 2500 metres overnight and then rise up close to 3000 metres on Saturday. Another 5-7 mm during the day on Saturday with strong Southwest winds, and then another 3-5 mm by Sunday morning. On Sunday the freezing level may start to creep down a bit in the alpine, but still very warm in the valleys. Forecast precipitation for Sunday and Monday are starting to look a bit lower, with only 2-3 mm expected on Sunday and 1-3 mm for Monday. Freezing level should remain close to 2400 metres on both days.

Avalanche Summary

Several natural wind slab avalanches were reported during and at the end of the storm that ended early Monday. On Monday one natural size 3 avalanche and one size 1.5 accidentally triggered avalanche were reported from the South Chilcotin Mountains. These were both wind slabs on northerly aspects near ridge top. Numerous size 1-2 loose wet slides were observed in the Coquihalla on Tuesday.

Snowpack Summary

New storm snow is sitting on a sun crust or surface hoar that caps the 30-50 cm of settling storm snow or faceted powder. Deep and dense wind slabs are likely bonding poorly to another hard crust and/or surface hoar layer in exposed wind-affected terrain. The bond to the crust could be somewhat variable but many observers report a good bond. Where surface hoar is present (possibly above the crust) the storm slab has been more reactive to ski testing on steep unsupported features. Deeper snowpack weaknesses are still on our radar, but seem to be dormant for the time being.

Regions covered