Lawinenlagebericht

South Rockies

Dec 22 – 23, 2013Avalanche Canada
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Archiviert · abgelaufen 13 years ago

Lawinengefahr

Tue
Wed
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering
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Kernpunkte

Check out the South Rockies Blog for more detailed up-to-date information.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    1–2
    Light amounts of new snow may have been shifted into pockets of small windslab at upper elevations. Watch for triggering in the lee of ridgecrests and terrain breaks.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–4
    The most significant interface is a layer of surface hoar buried in early December. It's buried 30-70 cm below the surface and is becoming more reactive in areas where the upper slab has become a little denser.

Confidence

Fair - Due to the number of field observations

Weather Forecast

Sunday night and Monday morning: Light snowfall / Moderate southwest winds with extreme gusts / Freezing level at 1300mTuesday: Mix of sun and cloud / Light winds /Freezing level at or near surfaceWednesday: Mix of sun and cloud / Light winds / Freezing level at or near surface

Avalanche Summary

A few loose dry sluffs from steep headwalls were observed in the past few days. In the southeast corner of the region explosives control produced a size 2 wind slab avalanche on a southeast facing slope.

Snowpack Summary

There appears to be a lot of snowpack variability across the region. Snowpack depths at treeline seem to vary from 50 - 110 cm with high variability in wind-exposed areas. Light amounts of new snow have fallen in the last few days and may have been shifted into small wind slabs in exposed areas. Located just below the surface is a layer of weak faceted crystals which formed during the cold snap at the beginning of December. At this point, there does not seem to be enough of an overlying slab to create a widespread problem. In the mid pack is the late-November/early-December interface which is made up of surface hoar, a crust, and/or facets. This layer is typically down 30-70cm and is most likely to pose the biggest problem for the region at the moment. Check out this video of a recent snowpack test on this layer. Despite its reactivity in snowpack tests, we have not yet seen widespread avalanche activity on this layer. I suspect it only needs a little more additional load to turn this into a more serious avalanche problem. A buried crust from mid-November can be found near the base of the snowpack below 1650 m and is breaking down into facets.

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