Bollettino valanghe

Northwest Inland

Feb 6 – 7, 2015Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 12 years ago

Pericolo valanghe

Sun
Mon
Alta quota
4 · Forte
Limite del bosco
3 · Marcato
Sotto il limite
3 · Marcato
Apri la mappa completa

In sintesi

There's fresh snow and clearing skies in store for the weekend which sounds amazing, but we need to SLOW IT WAY DOWN and stick to conservative terrain as the snowpack adjusts to the recent load.

Problemi valanghivi

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    2–7
    Snowfall should taper before dawn Saturday morning, but I suspect there is still potential for natural avalanche activity Saturday as a strong SW wind blows and the snowpack adjusts to the new load.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    4–7
    There's a lot of uncertainty surrounding the deeply buried weak layers in the snowpack. This weekend I would make decisions based on the assumption that every slope above treeline has the potential to produce a very large and destructive avalanche.

Confidence

Poor - Due to the number of field observations

Weather Forecast

Snowfall should slowly taper overnight. I'm expecting 5 to 20cm out of this last push. Winds should ease back (slightly), but I'm still expecting strong SW winds in the alpine Saturday. No snowfall is expected on Saturday, Sunday or Monday. Looks like it goes clear and dry through at least Tuesday.

Avalanche Summary

With the intense storm obscuring views, observations have been limited. I expect there is a widespread natural avalanche cycle occurring, we'll probably learn more about it as skies clear this weekend.

Snowpack Summary

The storm has produced approximately 20 to 50 cm of new snow accompanied by strong to extreme winds out of the E through SE. There are a number of weak layers in our snowpack, this storm should be a good test for all of them. In places the new storm snow sits on the early February surface hoar, little is known about the distribution of this interface. The late January crust is probably down 60 to 100cm in the south, it's likely shallower in the north. The mid-January rain crust(with some spatially spotty surface hoar on top) is down over a meter. It might still be a problem in thin snowpack areas. The crust/facet combination from November can be found near the ground. It's not an easy snowpack to work with, we'd greatly appreciate your observations via the Mountain Information Network.

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