Bollettino valanghe

Northwest Inland

Feb 28 – Mar 1, 2013Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 14 years ago

Pericolo valanghe

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

In sintesi

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–5
    Strong winds throughout the region have likely set up touchy wind slabs in the lee of ridges and terrain features. Watch also for growing cornices.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–5
    Storm slabs remain in the west and the south of the region where there were deeper recent snow amounts.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Synopsis: Residual moisture from the last Pacific system will give generally light amounts until Sunday, when a clearing trend develops.Friday: Most likely light snowfall (2-4 cm), but moderate snowfall possible in higher snow areas. Southwest winds 30 km/h. Freezing level around 800 m.Saturday: Light snow, 2-4 cm. Light winds. Freezing level around 600 m.Sunday: Dry and bright. Light northerly winds. Freezing level around 600 m.

Avalanche Summary

Small (size 1) soft slab avalanches could be triggered in response to ski-cutting at treeline on Wednesday; similar activity was reported on Tuesday and Monday from steep wind-loaded features. During the weekend there were reports of natural avalanches up to size 2.5 on north facing slopes following loading from new snow and wind.

Snowpack Summary

Recent storm snow amounts are 30-40 cm in the west of the region and more like 10 cm in the east. Strong southwest winds have formed touchy wind slabs in exposed terrain in the lee of ridges, gully side walls, and behind terrain features. There are a variety of old interfaces now down 60 - 100cm which include facets, crusts and isolated pockets of surface hoar. Recent observations indicate that these weaknesses have bonded fairly well now, but I still suggest digging and testing the snowpack to confirm.A strong mid-pack currently overlies a weak base layer of facets/depth hoar. It is worth noting that the snowpack in general is quite shallow in northern and eastern parts of the region. Triggering the basal weakness may still be possible from thin spots, rocky outcrops or under the weight of larger triggers such as cornice fall.

Regioni coperte