Bollettino valanghe

Northwest Inland

Mar 2, 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

Strong to Extreme winds accompanied by 5-10 cm will likely build reactive wind slabs. Deeper slabs may exist on leeward slopes.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely - Very Likely
    Dimensione
    1–2
    Strong to extreme SW winds and new snow will build fresh wind slabs on leeward slopes and behind terrain features. Loose dry avalanches may be easily triggered below treeline or in areas sheltered from the wind.

  • Deep Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Unlikely
    Dimensione
    2–4
    A lingering weakness at the bottom of the snowpack may remain sensitive to human triggering, especially in shallow snowpack areas. Smaller avalanches in motion also have the potential to step down and trigger deep persistent slabs.

Confidence

Moderate - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Wednesday night-Thursday: snow amounts 5-10 cm with light winds gusting extreme from the SW. Alpine temperatures near -3 and freezing levels 1000 m. Friday: Periods of snow 2-7 cm. Ridgetop winds light gusting to 65 km/hr from the SW. Alpine high of -8 and freezing levels falling to 500 m. Saturday: Mostly cloudy with sunny periods. Ridgetop winds generally light. Alpine temperatures high of -10 and freezing levels at valley bottom.

Avalanche Summary

On Tuesday, no new avalanche activity was reported. With forecast snow and strong winds, reactive wind slabs are likely over the next several days.

Snowpack Summary

New snow 5- 15 cm accompanied by strong- extreme SW winds is burying a plethora of old snow surfaces including isolated wind slabs and wind press, sun crusts, and surface hoar. The new snow may have a poor bond to these interfaces. At treeline elevations the average snowpack depths are 150-190 cm and a well consolidated mid-pack of approximately up to 100 cm sits above weak basal facets (sugary snow) near the ground. Recent snowpack testing has shown sudden results down 100 cm within the facetted snow. Although possibly a low probability for triggering the persistent slab exists, the consequence would be high as it has the potential to produce very large destructive avalanches especially in shallower snowpack areas.

Regioni coperte