Lawinenlagebericht

Cariboos

Feb 27 – 28, 2012Avalanche Canada
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Archiviert · abgelaufen 15 years ago

Lawinengefahr

Wed
Thu
Hochgebirge
3 · Erheblich
Waldgrenze
3 · Erheblich
Unterhalb
3 · Erheblich
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Kernpunkte

In your local area: Be wary of any slopes which are being warmed by direct sun, as this may weaken existing slabs and could cause natural avalanches.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–6
    Wind slabs have grown large on a variety of slopes. Persistent weak layers are buried beneath these slabs, meaning they could be touchy and create very large avalanches. Large cornices also threaten many slopes.

  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely
    Größe
    2–7
    Several weaknesses exist in the upper metre of the snowpack. These layers remain very sensitive. Large, destructive avalanches could be triggered by the weight of a person, even from a distance.

Confidence

Good

Weather Forecast

Tuesday: Mainly sunny with valley cloud. Light southerly winds. Freezing level around 600m. Wednesday/Thursday: Cloud and flurries. Light south-west winds. Temperatures remaining cool, except where sunny breaks are occurring and some local solar warming could occur.

Avalanche Summary

An avalanche cycle which began on Wednesday has slowed slightly with time, but conditions remain touchy with natural, human and remotely-triggered avalanches in the size 1.5-3 range reported most days. These are running on storm snow weaknesses or on buried weak layers in the upper snowpack. As snowfall and wind-loading ease over the next few days, expect natural avalanches to decrease, but tricky and touchy conditions for human-triggering to continue.

Snowpack Summary

Deep wind slabs exist on many aspects. Storm snow totals range from about 60-140cm above the Feb 16. surface hoar layer and the early Feb. surface hoar/ crust. The early Feb. surface hoar layer is widespread in some areas, while in others it's confined to shady aspects at treeline and in the alpine. A buried melt-freeze crust can be found on solar aspects at all elevations, and on all aspects below about 1600m. Snowpack tests on upper snowpack layers generally give easy to moderate "pops or drops" results. Ongoing remote and natural triggering further indicates the touchy nature of these weaknesses. Large cornices exist, which could trigger large avalanches on the Jan. 20th facet layer if they fall. Shallow snowpack areas may still harbour basal facets.

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