Bollettino valanghe

Northwest Inland

Mar 13 – 14, 2012Avalanche Canada
Vedi sulla mappa
Archiviato · scaduto 15 years ago

Pericolo valanghe

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

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–4
    Fresh windslabs may exist on lee slopes adding to a strengthening, yet widespread hard wind slab problem that developed last week.

  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1–5
    Large cornices exist in alpine terrain. A failure could be destructive by itself, and could also trigger an avalanche on the slope below.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–5
    The persistent weak layer that formed in early February is most prominent on unsupported, sheltered slopes at treeline . Although avalanches on this layer have not been reported this week, triggering may still be possible in isolated terrain.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

Wednesday: light snowfall - light southeast winds - freezing level at 600m Thursday: moderate snowfall - light to moderate south winds - freezing level at 900m Friday: light snowfall - light to moderate southwest winds - freezing level at 700m

Avalanche Summary

A few natural slab avalanches to size 2 occurred in response to recent wind loading in the north of the region. They occurred on steep, lee slopes behind ridges or cornices.

Snowpack Summary

Light amounts of low density snow sit over a variety of old surfaces that include widely distributed hard wind slabs, or melt freeze crusts that exist on most aspects below 1000m and on solar aspects as high as 1600m. In exposed areas the newer low density snow has been shifted into stiffer pockets of soft wind slab. The mid February interface, down around 60cm, is variable and generally consists of a strong melt freeze crust below 1000m. Above that elevation, expect to find buried facets, and/or surface hoar (in more sheltered areas), and/or a sun crust on southern aspects. The surface hoar is not widespread and is gaining strength, but should still be on your radar in steeper, unsupported terrain at treeline and below. Cornices in the area are also reported to be very large and primed for triggering.

Regioni coperte