Lawinenlagebericht

Purcells

Jan 8 – 9, 2013Avalanche Canada
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Archiviert · abgelaufen 14 years ago

Lawinengefahr

Thu
Fri
Hochgebirge
4 · Gross
Waldgrenze
4 · Gross
Unterhalb
3 · Erheblich

Kernpunkte

Cautious travel practices, and conservative decision making is essential through the forecast period.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely - Very Likely
    Größe
    1–6
    The consistent strong winds mean that the windslabs extend lower into the terrain than normal.
  • Cornices

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible - Likely
    Größe
    2–5
    Strong winds and lots of new snow makes perfect conditions for cornice growth. These are a hazard by themselves but can also trigger avalanches on slopes below.
  • Storm Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Likely
    Größe
    1–4
    As the storm snow gets deeper, the slab will become more cohesive and reactive.

Confidence

Fair - Forecast snowfall amounts are uncertain on Wednesday

Weather Forecast

Wednesday: Cloudy with lingering snowfall. Expect 20-40cm of total accumulations, with the higher amounts in the southern portion of the region. Winds should be strong southwesterlies with freezing levels climbing to 1300m.Thursday: There is a chance of continued flurries, with westerly winds abating and temperatures falling to -13.Friday: Expect mixed skies with light winds and cool temperatures.

Avalanche Summary

Small windslabs up to size 1.5 have been reported, failing in immediate lee locations of ridgelines and isolated storm slabs have been reported to 1.0. Sluffing up to size 1.5 continues.

Snowpack Summary

On the west side of the region up to 50cm of new snow overlies the January 4th interface while on the east side the new snow totals around 10-20cm. Consistent moderate and strong south/southwest winds have redistributed this new snow into windslabs in lee features in the alpine and exposed treeline and these windslabs are reactive to human triggering. In some areas the windslabs extend lower down the slope than normal due to locally extreme winds.The January 4th interface consists predominantly of loose facets. In isolated locations (sheltered treeline and below treeline) surface hoar is present and there is a sun crust on steep south and west facing terrain. In some areas the new snow is bonding poorly to these interfaces, and lots of sluffing is being reported. Where the storm snow is deeper (around 30cm), the sluffing is extensive enough to require a management plan. The deepest deposits of storm snow (pushing 50cm) are settling into a more cohesive storm slab. The midpack is well bonded and strong. The deep crust/facet combo from early November still exists and concern remains (although unlikely) for triggering this layer from a shallow spot.

Abgedeckte Regionen