Lawinenlagebericht

South Columbia

Dec 24, 2018Avalanche Canada
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Archiviert · abgelaufen 8 years ago

Lawinengefahr

Tue
Wed
Hochgebirge
3 · Erheblich
Waldgrenze
2 · Mässig
Unterhalb
2 · Mässig

Kernpunkte

The persistent slab problem is best managed with patience and conservative terrain choices. Read more in the new forecaster blog here.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Watch for wind slabs in open and lee terrain.
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–3
    The likelihood of persistent slab avalanches is gradually decreasing, but triggering a widespread weak layer buried 50-100 cm beneath the surface has major consequences. This problem will likely linger through the holidays.

Confidence

High - Due to the number and quality of field observations.

Weather Forecast

SUNDAY NIGHT: Isolated flurries with localized accumulations of 2-5 cm, light wind from the southwest, alpine temperatures drop to -8°c. MONDAY: Mostly cloudy with a few sunny breaks, light wind, alpine high temperatures around -8°c. TUESDAY: Mix of sun and cloud, light wind, alpine high temperatures around -10°c. WEDNESDAY: Mostly cloudy, light wind, alpine high temperatures around -10°c.

Avalanche Summary

Preliminary reports from Sunday indicate the most recent 20 cm of new snow was reactive to skiers on steep and convex features. No significant avalanche activity was reported on Saturday, as natural and human triggered activity has started to tapered off. However, as recent as Friday, large (size 2-3) persistent slab avalanches were occurring naturally. There have also been a few notable persistent slab avalanches remotely triggered from skiers on adjacent slopes. Most recently, a few large (size 2-2.5) avalanches on north-facing slopes at treeline elevations were remotely triggered by skiers in the Selkirks on Wednesday.

Snowpack Summary

Recent wind from the southwest has formed wind slabs in the alpine and around treeline. A week of stormy weather has deposited 50-100 cm of snow above a weak layer of facets (sugary snow), surface hoar (feathery crystals), and a sun crust (on south aspects) that formed during the dry spell in early December. This layer has been responsible for large persistent slab avalanches over the past week, particularly on northeast facing slopes above 1900 m and on south-facing slopes in the alpine. The potential exists for smaller avalanches to step down and trigger this layer, resulting in very large avalanches. Another weak layer from mid-November is now buried up to 120 cm, but has been less active recently. At the base of the snowpack is a crust that formed in late October.

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