Bollettino valanghe

Kootenay Boundary

Dec 1 – 2, 2013Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 13 years ago

Pericolo valanghe

Tue
Wed
Alta quota
4 · Forte
Limite del bosco
3 · Marcato
Sotto il limite
2 · Moderato
Apri la mappa completa

In sintesi

New snow and wind are increasing the avalanche danger. Storm slabs may release naturally or be triggered by light additional loads like skiers/riders.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–5
    I have this problem on all aspects, because we do not have many reports from this region. Dig down and find out if this deeply buried weak layer is in your area. Let us know what you find.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    1–5
    New storm slabs may release naturally or be triggered by light additional loads like skiers/riders. These storm slabs may be sitting on a layer of surface hoar on Northerly aspects, or on a melt/freeze crust on Southerly aspects.

Confidence

Poor - Due to the number of field observations

Weather Forecast

Overnight and Monday: 15-30 cm of snow overnight as the cold arctic air from the North meets the warm moist Pacific air crossing from the West. The mountain passes in the South of the region may see higher snowfall amounts.  Freezing levels dropping to valley bottoms and winds becoming moderate from the Northeast by Monday afternoon.Tuesday: Cold and dry with light Northerly winds.Wednesday: Sunny, dry and cold.

Avalanche Summary

The new storm snow is expected to release naturally or with light additional  loads like skiers. Areas that have a deeply buried early season crust may experience a cycle of large avalanches due to the added load of the storm snow.

Snowpack Summary

New storm slabs are developing above recently buried weak layers of surface hoar on North aspects and melt/freeze crusts on solar aspects. The new snow may not bond well to these old weak surface layers. There are some reports of a deeply buried early season crust that formed in October. We do not know the extent of this layer with respect to aspect and areas within the region. In other regions of the interior mountains, this layer is more likely to be found in the high alpine on northerly aspects.

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