Bollettino valanghe

Northwest Inland

Mar 14 – 15, 2017Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 10 years ago

Pericolo valanghe

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

In sintesi

Stormy weather continues to keep the avalanche danger elevated. Watch for deep pockets of wind transported snow at higher elevations.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    2–3
    A reactive slab has possibly formed above a weak layer of crusts, facets, and surface hoar that formed in February. This weak layer may be spotty and confined to terrain that is sheltered from the wind.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2
    Storm slabs are expected to continue to develop due to forecast new snow and wind. Watch for the transition to moist or wet snow as you descend in elevation.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely - Possible
    Dimensione
    2–3
    A lingering weakness at the bottom of the snowpack may reawaken with the load of the new snow and warming. It'll be most reactive in thin rocky start zones and shallow snowpack locations.

Confidence

Moderate - Forecast snowfall amounts are uncertain on Wednesday

Weather Forecast

Overnight: Freezing level dropping to valley bottoms, and 3-5 cm of new snow combined with strong southwest winds. Wednesday: Moderate southwest winds, daytime freezing level around 700 metre, and flurries or periods of light snow. Thursday: Moderate southerly winds, freezing at valley bottoms, and 3-5 cm of new snow. Friday: Moderate southerly winds, freezing level at valley bottoms, and 3-5 cm of new snow.

Avalanche Summary

Numerous natural avalanches up to size 2.5 were reported from the west of the region in the Howson's.

Snowpack Summary

Storm slabs continue to build with each pulse of snow and wind. Warm temperatures will make touchy slabs at higher elevations and unstable wet snow at lower elevations. A weak interface that was buried in late February may finally have enough snow above it to form a reactive slab. The interface is composed of facets, crusts, and surface hoar and may be 40-80 cm deep. There's uncertainty about the distribution and reactivity of this interface. The mid-pack is well consolidated and sits above weak sugary snow near the ground. The deeper basal weakness remain a concern in thin rocky start zones and shallow snowpack locations.

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