Bollettino valanghe

Purcells

Nov 25 – 26, 2015Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 11 years ago

Pericolo valanghe

Fri
Sat
Alta quota
Senza grado
Limite del bosco
Senza grado
Sotto il limite
Senza grado
Apri la mappa completa

In sintesi

Forecasters are working with a scarcity of information at this time. Use caution in this early season snowpack and take the time to dig a pit. We'd love to hear from you if you have information to share on the Mountain Information Network. MIN

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–3
    Winds out of the north are building wind slab formations on southerly features. These slabs will be most problematic immediately lee of ridge crest, but you may encounter them in the right feature at treeline as well.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely
    Dimensione
    4–6
    November weak layers may be less reactive, but it's important to remember that there may be a weak layer of crust and facets near the ground. Most likely to be found on north through east facing alpine features.

Avalanche Summary

One operator produced a size 2 avalanche with explosives on a N slope at 2300m. There have also been reports of skier controlled size 1's, 15 to 20cm storm slabs failing on the Nov 23rd surface hoar

Weather Forecast

Arctic air has moved in from the north bringing clear skies and cooler than average temperatures. Strong northerly winds at ridge top are expected to continue through Thursday afternoon, and then back off to more moderate speedsby Friday after whichwinds should diminish to lighter values. Above freezing temperatures in the alpine are forecast to begin Friday morning and continue into the weekend but valley bottoms will remain well below freezing.

Snowpack Summary

Monday's storm snow fell on a variety of old surfaces including crust, surface hoar and old settled snow. Arctic air moving into the region has resulted in northerly winds which have formed small wind slabs on south facing features near ridge top. Warm temps and strong solar input formed a crust on south facing features which can be found underneath Monday's storm snow. There are at least three surface hoar layers in the snowpack buried on: Nov. 5th, Nov. 11th and Nov. 23rd. The first two have been largely unreactive. Facets may exist just above the ground on shaded slopes in the alpine.  Warming temperatures  in the alpine for later in the week may significantly change the alpine hazard

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