Bollettino valanghe

South Coast

Jan 29 – 30, 2016Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 11 years ago

Pericolo valanghe

Sun
Mon
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole
Apri la mappa completa

In sintesi

Destructive persistent weak layers should still be on your radar if you're heading to the north of the region.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–3
    New snow and wind over the next few days will form new wind slabs in high elevation lee terrain. Watch for triggering in gullies and behind ridge crests.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–3
    Recent stormy weather has encouraged widespread cornice growth. Large cornice falls can be destructive by themselves, but can also be a trigger for surprisingly large avalanches on the slope below.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–6
    In many areas, buried persistent weaknesses have been destroyed by recent wet and stormy weather. I'd still be cautious in high elevation terrain (particularly in the north of the region) as the snowpack adjusts to the weight of the new snow.

Confidence

Moderate - Due to the number of field observations

Weather Forecast

Expect 5-15cm of new snow to fall between Friday night and Saturday. An additional 5cm may fall on Sunday, while isolated flurries and sunny breaks are forecast for Monday. Winds on Saturday will be strong from the southwest, and then drop to light and northwesterly for Sunday and Monday. Freezing levels should hover between 500-700m for the entire forecast period.

Avalanche Summary

On Thursday, persistent and storm slab avalanches to size 3.5 were observed on a variety of aspects and elevations. They occurred in response to heavy storm loading from rain and snow. The mid-January surface hoar was the suspected culprit in many of these avalanches. Of note was a size 4 slab avalanche in Steep Creek in the Duffey Lake area. Thanks to the individual who submitted this great observation through the Mountain Information Network. Moving forward, cooling will likely put a cap on persistent slab avalanche activity, except on higher elevation slopes in the north of the region where reactivity is expected to persist. Forecast wind and snow will spark a new round of wind slab activity in high elevation lee terrain over the weekend.

Snowpack Summary

On Wednesday night and Thursday morning, heavy snowfall and strong winds continued to form deep and dense storm slabs in high elevation terrain and cause substantial cornice growth. The snow line fluctuated a great deal during the storm which dropped around 80mm of precipitation throughout the region. At treeline and below, heavy rain saturated the snowpack. With forecast cooling, slopes at these elevation bands may now be sporting a hard crust. Where it still exists, the mid-January surface hoar layer is between 60 and 130 cm below the surface. The combination of heavy storm loading and warm temperatures has likely flushed out this weak layer in many areas. I would still exercise caution on higher elevation slopes in the north of the region where continued reactivity at this destructive interface is likely to persist. New snow and wind on Friday night and Saturday will form new wind slabs in high elevation lee terrain.

Regioni coperte