Boletín de aludes

Sea To Sky

Feb 22 – 23, 2016Avalanche Canada
Ver en el mapa
Archivado · caducó 11 years ago

Peligro de aludes

Wed
Thu
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil

Lo esencial

Avalanches will be more likely on slopes that see direct sun on Tuesday.

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1–4
    Cornices are reported to be large and weak. The weight of a person may be enough to cause a cornice failure.
  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    The recent storm slabs continue to be reactive to human triggering especially on wind loaded slopes. If the sun shines it may have enough punch to trigger natural avalanches.

Weather Forecast

TUESDAY: sunny, light southeasterly winds, 1500m freezing level. WEDNESDAY: partly cloudy with flurries possible, light southwesterly winds, 1500m freezing level. THURSDAY: mainly sunny, light southwest winds, freezing level rising to 3000m.

Avalanche Summary

Numerous natural and artificially triggered storm slab avalanches were reported over the weekend. Although natural avalanche activity is now slowing, wind slab avalanches are expected to remain reactive to human-triggering. Cornices are reported to be large and fragile, and may fail under the weight of a person.

Confidence

High - Due to the number and quality of field observations

Snowpack Summary

The recent storm snow continues to settle and gain strength, however, some lingering mid storm instabilities are still reactive to ski cutting in steeper terrain features. Ongoing southeast through southwest winds have been loading lee features in the alpine and at treeline and cornices are large and fragile. A thin breakable crust may cap moist snow on slopes that see direct sun. Several crusts can be found in the upper meter depending on elevation and aspect. The upper snow pack is sitting on a more widespread and thicker crust that extends into the alpine. In most places this crust is bridging a layer of surface hoar buried in early January. It is becoming increasingly hard to make this layer fail in snowpack tests and triggering an avalanche on it is unlikely.

Regiones cubiertas