Bollettino valanghe

Northwest Coastal

Jan 19 – 20, 2013Avalanche Canada
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Archiviato · scaduto 14 years ago

Pericolo valanghe

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

In sintesi

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–5
    Strong to extreme westerly winds have continued to create windslabs in exposed lee and cross-loaded terrain at higher elevations. Heavy accumulations in the north have created a very destructive storm/ windslab instability.

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–6
    There has been no new activity reported on this layer. Having said that, the weakness still exists with the potential to produce large avalanches.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–4
      Forecast warm temperatures and the possibility of sun will increase the likelihood of loose wet avalanche activity. Watch for triggering in steep, sun exposed terrain.

Confidence

Fair - Due to variable snowpack conditions

Weather Forecast

The stationary ridge of high pressure is expected to bring continued dry conditions to the region until Tuesday at which point the ridge moves east allowing light snowfall to affect westerly slopes. Alpine temperatures are forecast to be about 0.0` for Sunday and Monday, and then dropping on Tuesday. Winds should remain light to moderate from the southwest.

Avalanche Summary

On Thursday and Friday numerous avalanches ran to size 3.5 in the north of the region where recent snow accumulations were the highest. They occurred in response to heavy snowfall and strong to extreme winds. Most recent occurrences were observed on east to northwest aspects at treeline and above. One result pulled down to basal weaknesses where it interacted with summer firn.

Snowpack Summary

A melt freeze crust is likely to exist in most areas below treeline that were previously rain soaked. Light amounts of recent snow (heavy amounts in the north) exist as storm slabs and windslabs at treeline and above. A persistent weakness of surface hoar buried at the end of December sits below all of the more recent storm snow and is still on the radar of professionals in the area. The mid and lower snowpack is generally well settled and strong, although well developed basal facets remain a concern in shallow snowpack areas.

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