Lawinenlagebericht

Sea To Sky

Nov 30 – Dec 1, 2012Avalanche Canada
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Archiviert · abgelaufen 14 years ago

Lawinengefahr

Sun
Mon
Hochgebirge
4 · Gross
Waldgrenze
3 · Erheblich
Unterhalb
2 · Mässig
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Kernpunkte

Lawinenprobleme

  • Storm Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely - Very Likely
    Größe
    1–5
    New snow at upper elevations continue to build storm and wind slabs overlying a variety of weak surface layers. Natural and rider triggered avalanches are likely; especially on lee slopes, and behind terrain features that have been wind loaded.

  • Deep Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Unlikely - Possible
    Größe
    2–6
    Slopes with smooth ground cover and reloaded bed surfaces may be prone to remote triggering and step down avalanches. Typical trigger points include thin rocky areas. May be difficult to trigger, but often very large with serious consequences.

Confidence

Poor - Timing, track, or intensity of incoming weather is uncertain for the entire period

Weather Forecast

The deep low pressure system off the Gulf of Alaska continues to spin a moist, warm southwesterly flow over the South Coast mountains. The weather pattern will remain continuous and active through the forecast period. Saturday: FLVL’s 1200 m, snow amounts 10-15 cm, ridgetop winds SE 40-50 km/hr, alpine temps near -4.Sunday: FLVL’s 1200m, snow amounts 5-10 cm, ridgetop winds S 10 km/hr, alpine temps -4.Monday: FLVL’s 1100 – 1400m, snow amounts 5-10 cm ridgetop winds S 35 km/hr, alpine temps -5.

Avalanche Summary

Explosive testing produced numerous size 1-1.5 slab avalanches on NW-N aspects. All instabilities reacting within the storm snow.

Snowpack Summary

The region will continue to see moderate amounts of new snow, and strong SW winds. Storm slabs and fresh wind slabs will load a variety of weak surfaces. These (now buried) surfaces consist of large surface hoar, a thin sun crust, and surface facets. Below this, the mid-pack seems to be fairly settled, strong and bridging instabilities that may exist deeper.Under the mid-pack (90-150 cm down) sits the early November facet/ crust persistent weakness. Recent snowpack tests have shown sudden collapse (or "drops") results on the early November facet/crust deep persistent weakness, but because this weakness is so close to the ground in most areas, associated avalanche activity will likely be limited to slopes with smooth ground cover (e.g. scree slopes, rock slabs, summer firn, glaciers, etc.). Areas that are most susceptible to trigger this deep persistent weakness are shallow, thin and variable snowpack deposition spots.To view a recent snow pit profile from the Spearhead Range, check out the Wayne Flann Avalanche Blog.

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