Lawinenlagebericht

Northwest Coastal

Apr 11 – 12, 2015Avalanche Canada
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Archiviert · abgelaufen 11 years ago

Lawinengefahr

Mon
Tue
Hochgebirge
3 · Erheblich
Waldgrenze
3 · Erheblich
Unterhalb
1 · Gering

Kernpunkte

Wind effect in the alpine and a treeline are of prime concern with this storm, use caution when riding/traveling in the backcountry. If you have field observations to share here we'd love to hear from you.

Lawinenprobleme

  • Wind Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–3
    Strong winds associated with this storm have built wind slabs in lee terrain, these wind loaded pockets may be sitting on facets, surface hoar or crusts and could be very touchy
  • Persistent Slabs

    • Hochgebirge
    • Waldgrenze
    • Unterhalb der Waldgrenze
    Wahrscheinlichkeit
    Possible
    Größe
    1–4
    Additional loading on the March 25 combi-layer may make this layer extremely touchy. Use caution in wind loaded areas and other deep deposition zones.

Confidence

Fair - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

SUNDAY: Will ramp up precipitation with another 8 to 10 cm of snow at upper elevations. Freezing levels 500m overnight to 800m with daytime heating. MONDAY: Another 5 to 10 cm of snow. Precipitation will be heavier towards the coast, but the inland portion of the Northwest Coast may see as much as 45 cm of snow at upper elevations through the forecast period.TUESDAY: A brief break in the weather, cloudy with sunny periods, some flurries with freezing levels from 500 to 800m. Winds moderate to strong from the south west for the forecast period.

Avalanche Summary

Commercial operators are reporting strong winds in the alpine stripping the new snow down to old crust surfaces and building wind slabs and sastrugi. One operator has reported numerous size 2 and 2.5 avalanches with explosives control.

Snowpack Summary

New snow is being redistributed by strong south west winds into wind slabs on lee slopes. Reports of activity on the March 25th surface hoar / crust layer have diminished, but is still worth remembering. This interface was more reactive recently in the northern part of the region, but had been reported throughout the northwest coastal area and may reappear as a problem given the right conditions. For the most part, the chief concern is wind slabs over a variety of recent surfaces, crusts, facets and surface hoar that formed in in sheltered places during the last spell of clear cold weather. Large ripe cornices are also of concern with additional loading, especially when the sun and warm temperatures come back.

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