Lawinenlagebericht

Purcells

Apr 2 – 3, 2015Avalanche Canada
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Archiviert · abgelaufen 12 years ago

Lawinengefahr

Sat
Sun
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering

Kernpunkte

The persistent slab problem is still on the radar, but shifting into a low-probability/ high-consequence situation. Be confident in your local snowpack before committing to any big terrain.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Recent winds shifted dry new snow into wind slabs on lee and cross loaded slopes. Cornices may be large and fragile.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–5
    Buried persistent weak layers may still be reactive to human-triggering and large avalanches remain possible. Smaller avalanches in motion or a cornice failure could step down to one of these deeper layers.

Confidence

Fair - Forecast snowfall amounts are uncertain

Weather Forecast

Light snow starts on Friday night and continues through the weekend. (Estimates: 5 cm on Saturday; 1-5 cm on Sunday; 5 cm on Monday). The freezing level is around 1500 m by day, falling towards valley floor by night. Winds are generally light.

Avalanche Summary

Ongoing persistent slab, storm slab, and loose wet avalanche activity has tapered off recently. While the likelihood of triggering a large avalanche has gone down, the consequences remain high. On Wednesday, some natural cornice falls were observed on shady aspects, some of which triggered slabs up to size 2.5 on the slopes below. Isolated wind slabs were also reported.

Snowpack Summary

Recent 10-25 cm snow was shifted by variable strong winds into wind slabs on lee slopes above about 2000 m. Cornices are large and touchy in some spots. The new snow sits over various crusts which formed recently. Low elevations sport an isothermal snowpack, which may now be capped by a refrozen crust.Several persistent weak layers exist in the upper 1m of the snowpack and remain a concern. In the north of the region, the mid-March crust/facet layer is down 40-60cm and remains an isolated concern. Just below this layer is the mid-February crust/facet/surface hoar layer, which may also still be reactive in isolated areas. Both layers have the potential for wide propagations and large avalanches are still possible.

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