Bollettino valanghe

North Columbia

Jan 2, 2018Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 9 years ago

Pericolo valanghe

Wed
Thu
Alta quota
3 · Marcato
Limite del bosco
3 · Marcato
Sotto il limite
3 · Marcato
Apri la mappa completa

In sintesi

Rapid warming is expected in the alpine, while persistent slab problems exist at treeline and below. Safe travel requires careful route selection. Steep, open or sparsely treed slopes are best avoided at this time.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–3
    A weak layer of surface hoar buried 50-80 cm deep has potential to be reactive in areas where the overlying snow has settled into a cohesive slab.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–2
    With expected warm temperatures, recent storm snow will settle into a denser slab, making triggering avalanches in steep terrain more likely. Especially at treeline, a small initial slide could step down to the persistent weak layer below.

Confidence

High -

Weather Forecast

Tuesday: Cold air in the valleys, warmer air up high. An above freezing layer is expected from approximately 2000-2500 m. Some valley cloud is possible, clear at upper elevations. Light westerly winds.Wednesday: basically a repeat of Tuesday, possibly slightly warmer.Thursday: Cloud developing. Lower elevations are finally expected to start to warm, although the above freezing layer is expected to remain in place. Light southwesterly winds.

Avalanche Summary

There have been a several recent reports of remote-triggered (triggered from a distance) persistent slab avalanches to size 2 on west, south and northerly aspects between 1400-1800m. Reactivity on the persistent slab is likely to increase with warmer temperatures as the upper snow becomes denser.

Snowpack Summary

30-50cm of low density new snow from last week has buried a layer of weak feathery surface hoar and/or sugary facets. This new snow is expected to start to consolidate into a slab once forecast warmer temperatures take effect, but so far the upper snow has been remained light and soft. Of greater concern is a weak layer buried mid-December that consists of surface hoar, a sun crust and/or sugary facets, and is now down approximately 50-70cm.The bond at this interface is highly variable. The most concerning areas are those that saw pronounced surface hoar development before mid-December, such as sheltered areas at and below treeline, sheltered northerly aspects in the alpine, or anywhere the surface hoar formed on top of a sun crust. Recent snowpack tests show wide ranging reactivity on this weak layer but suggest that it may be most reactive on northerly aspects. A rain crust that formed in late November is now buried 80-120cm deep. Treeline snow depths are in the region of 200 cm.

Regioni coperte