Bollettino valanghe

Kootenay Boundary

Mar 18 – 19, 2016Avalanche Canada
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Archiviato · scaduto 11 years ago

Pericolo valanghe

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

In sintesi

With warming temperatures, avalanches may run naturally, especially on steep sun affected slopes. Cornices have grown large and will weaken with rising temperatures. Be conservative with terrain choices.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    3–5
    Surface hoar buried down about one metre has been recently triggered by light loads like a single skier or rider. Strong solar radiation and warm daytime temperatures may increase the likelihood of triggering.

  • Storm Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible - Likely
    Dimensione
    1–4
    Recent storm slabs and cornice growth continue to be a concern for human triggering. Forecast strong solar radiation may increase the reactivity of the slab and the likelihood of triggering large destructive avalanches.

  • Loose Wet

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–3
    Strong solar radiation and warm temperatures may result in loose wet snow releasing naturally from steep terrain. A skier or rider may also trigger a loose wet avalanche that could affect buried weak layers and trigger a large destructive avalanche.

Confidence

Moderate - Timing or intensity of solar radiation is uncertain on Sunday

Weather Forecast

The ridge will remain in place through Saturday as a southwesterly flow brings warm air into the region for Saturday and Sunday. FRIDAY: The freezing Level is forecast to climb above 1500 m, returning to valley bottom overnight, light easterly winds, with no precipitation forecast. SATURDAY: Freezing level starting at valley bottom climbing to 2500 m in the afternoon, light to moderate southwest winds, no precipitation. No overnight temperature recovery expected. SUNDAY: Freezing level holding at 2500 m, moderate southwest winds at ridge top, light precipitation expected. Increasing cloud cover will likely trap warm air leading to a greenhouse situation. 

Avalanche Summary

It's been a very active period with numerous large natural and human triggered avalanches being reported over the last few days. On Wednesday a skier remote triggered a cornice failure from a few meters away on a north/northeast facing slope around 2100 m in the Rossland range. When the falling chunks of cornice impacted the slope below it triggered a very large (size 3) avalanche that ran on the March 6th crust. Natural cornice failures were also reported. A second skier triggered avalanche (size 2) was reported on a northeast facing feature near 2000 m. Numerous loose wet avalanches to size 1.5 were also reported from solar aspects. ( facing southerly) On Monday a sleddder triggered a size 2 avalanche on a north facing feature at 1900 m failing on the late February surface hoar which resulted in a fatality in the Mt. Mackie area southwest of Castlegar.

Snowpack Summary

The recent storm snow of 40 to 60 cm continues to settle above a mix of crusts at treeline and below. In some drainages these storm slabs may be sitting on a thin crust that was initially buried on March 11th. A second crust, (the early March melt/freeze crust) can be found down 50 to 80 cm. The late February (Feb 27th) persistent weak layer of buried surface hoar down is now down 70 to 120 cm and has been the interface for some large avalanches. I suspect that this weak layer is more prominent on northerly (shaded) aspects at and above 1700 m. This surface hoar layer may also be associated with a crust on solar aspects. With the forecast of sun and strong solar radiation, triggering this deep weak layer may become easier. Pay attention to moist or wet surface snow as a sign that solar radiation is strong and deep weak layers may become reactive.

Regioni coperte