Avalanche forecast

South Rockies

Dec 19 – 20, 2013Avalanche Canada
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Avalanche danger

Sat
Sun
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
1 · Low
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Highlights

Avalanche problems

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–3
    Wind slabs in the alpine and open areas at treeline remain the primary problem throughout most of the region.

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Unlikely - Possible
    Size
    1–4
    A variety of PWLs are still being discussed across the region including the Oct crust, the mid-Nov crust, and the early-Dec surface hoar. These layers are generally inactive or stubborn to trigger but may still pose a problem in isolated areas.

Confidence

Poor - Due to the number of field observations

Weather Forecast

A low pressure system moves into the interior on Friday but it will be very weak or may not even reach the S. Rockies.  It will result in unsettled but generally benign conditions for the weekend.Friday: A mix of sun and cloud, very light snowfall possible late in the day, treeline temperatures around -10C, light SW/W windsSaturday/Sunday: A mix of sun and cloud, mostly dry conditions but very light snowfall possible, treeline temperatures around -10C, light winds

Avalanche Summary

No new avalanches reported.

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. There are several persistent weak layers which are still being discussed in the region. There is a lot of uncertainty as to the reactivity of these layers and it may vary across the region. We highly recommend digging and investigating these layers in your local area before exposing yourself to avalanche terrain. Nearest to the surface is the mid-December (~Dec 10) facet/surface hoar/crust interface which does not seem to have enough snow on it yet to create a widespread problem. Next 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. The mid-November crust is likely in the middle of the snowpack and may be faceting. Near the base of the snowpack is the early-Oct crust/facets and potentially depth hoar which may still have the potential to create avalanche problems, especially in thin snowpack areas.

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