Lawinenlagebericht

South Rockies

Dec 27 – 28, 2013Avalanche Canada
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Archiviert · abgelaufen 13 years ago

Lawinengefahr

Sun
Mon
Hochgebirge
2 · Mässig
Waldgrenze
2 · Mässig
Unterhalb
1 · Gering
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Kernpunkte

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

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–2
    Recent strong winds have redistributed loose surface snow into pockets of wind slab at many elevations. Wind slabs may be gaining strength, but triggering is still possible in unsupported terrain.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–4
    A recent skier-triggered size 2 avalanche in the Harvey Pass area indicates persistent weaknesses buried at the end of November have become active. The variable nature of this instability requires an investigative approach for safe mountain travel.

Confidence

Fair - Due to the number of field observations

Weather Forecast

Saturday: Mainly sunny skies / Light winds / Freezing level at 1200mSunday: Light flurries / Moderate west winds with extreme gusts / Freezing level at 800mMonday: Light snowfall / Moderate west winds with extreme gusts / Freezing level at 1600m

Avalanche Summary

On Christmas Eve a backcountry skier triggered a size 2 slab avalanche on an alpine slope in the Harvey Pass area. The slab was reportedly 70cm deep and 150m wide and was thought to have slid on the late-November crust/facet interface. There were no reported injuries with the avalanche.No other avalanches have been reported.

Snowpack Summary

There appears to be a lot of snowpack variability across the region. Snowpack depths at treeline seem to vary from 60 - 130 cm with high variability in wind-exposed areas. Mostly modest amounts of low density snow have fallen over the last week and have been shifted into small wind slabs in exposed areas. In some areas rain has created wet snow surfaces below treeline. 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 has reached the tipping point for rider triggering in a few areas including the Harvey Pass area. Check out this video of a recent snowpack test on this layer.

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