Boletín de aludes

Northwest Coastal

Apr 2 – 3, 2013Avalanche Canada
Ver en el mapa
Archivado · caducó 13 years ago

Peligro de aludes

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

Lo esencial

Problemas de aludes

  • Cornices

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–6
    Large developed cornices loom over slopes. A cornice fall has the potential to initiate large avalanches.
  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–5
    Reports of remote triggering suggest the March 9th surface hoar layer is still touchy in some areas. Where it is still reactive, avalanches can be large and potentially destructive.
  • Loose Wet

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–4
    Loose wet avalanches are likely on steep south facing slopes during the day if the sun is shining.

Confidence

Fair

Weather Forecast

Synopsis: The upper ridge of high pressure rebuilds on Wednesday resulting in more sun through Thursday morning. The ridge gives way to a low pressure system later on Thursday bringing moderate precipitation and increasing winds. Wednesday: A mix of sun and cloud. The freezing level is around 1200 m and winds are light from the southwest.Thursday: Increasing cloud with light snow developing in the evening. The freezing level rises to 1400 m during the day and winds are generally light from the south. Friday: Moderate precipitation. The freezing level is near 1000 m.

Avalanche Summary

In recent days loose wet activity to size 2 has been observed in steeper sun-exposed terrain. Natural cornice releases to size 3 were also noted. A size 1.5 slab avalanche was also remotely triggered from 75m away. I would suspect the March 9th interface was the culprit with this event.

Snowpack Summary

Surface snow has settled with the influence of warm temperatures and surface faceting continues on steep shaded slopes. Solar aspects in the alpine and all lower elevation terrain are now well into a daily melt-freeze cycle with sun-exposed slopes becoming very weak with daytime warming.Between 50-75cm below the surface is layer of surface hoar buried on March 9th which is variably reactive. In some areas it is stubborn and requires a significant trigger. In other areas the layer is still well preserved showing sudden planar or sudden collapse test results, and remains a primary concern among some professional operators.The mid snowpack is generally well settled and strong. Having said that, basal facets may resurface as a concern with spring warming, particularly in the north of the region. Cornices are large and untrustworthy, especially when the sun is out.

Regiones cubiertas