Bollettino valanghe

Sea To Sky

Feb 9, 2018Avalanche Canada
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Archiviato · scaduto 9 years ago

Pericolo valanghe

Sat
Sun
Alta quota
3 · Marcato
Limite del bosco
2 · Moderato
Sotto il limite
1 · Debole

In sintesi

When the sun pokes out natural slab and loose dry avalanche activity will likely increase.

Problemi valanghivi

  • Wind Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Likely
    Dimensione
    1–2.5
    Wind slabs remain reactive to rider triggers, especially on leeward slopes and behind terrain features.
  • Cornices

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    1.5–2.5
    Large looming cornices exist along ridgelines. They require respect and discipline. Give them an extra wide berth from above and below.

Confidence

Moderate - Wind effect is extremely variable

Weather Forecast

Friday: A mix of sun and cloud with alpine temperatures near -9 and freezing levels dropping to valley bottom. Ridgetop winds light from the North.Saturday: Sunny. Alpine temperatures near -5 and freezing levels valley bottom. Light winds from the North.Sunday: A mix of sun and cloud. Alpine temperatures -7 and freezing levels rising to 800 m. Light winds from the northeast.

Avalanche Summary

On Thursday, avalanche control with explosives triggered numerous slab avalanches up to size 2. Cornice releases triggered wind slabs from the slopes below up to size 1.5. With colder temperatures expected this weekend, natural avalanche activity will likely taper off, but human triggering will be possible especially on leeward slopes and behind terrain features.

Snowpack Summary

Snow surfaces vary from aspect to elevation showing crusts, wind pressed and scoured conditions. In the alpine 5-15 cm of recent snow, accompanied by strong winds from the southeast have formed reactive wind slabs in leeward terrain and large looming cornices exist, they are fragile and demand respect. Treeline and below treeline elevations a melt-freeze crust has formed.An average of 170 cm of settled snow now sits on the mid-January crust which generally shows signs of bonding to the overlying snow; however, it has the potential to "wake-up" with a large trigger such as a cornice fall. Below this, the snowpack is thought to be generally strong and well-settled.

Regioni coperte