Boletín de aludes

Sea To Sky

Jan 3 – 4, 2016Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Tue
Wed
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil

Lo esencial

There's a lot uncertainty regarding the timing and intensity of snowfall forecast for Monday. When it does arrive, new wind slabs are expected to form.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–2
    New wind slabs are expected to form on Monday, although forecast snowfall amounts for the next few days are highly uncertain. Pay close attention to how much snow falls in your area, and choose terrain accordingly.

Confidence

Low - Timing, track, or intensity of incoming weather system is uncertain on Monday

Weather Forecast

There is a ton of uncertainty with the weather pattern over the next 48 hours as models are disagreeing on the timing, track and intensity of precipitation. The region could see anywhere from 0cm to 20cm between Monday and Tuesday. Ridgetop winds should be mainly moderate from the southeast. Freezing levels should sit around valley bottom on Monday, and rise gradually to about 1000m on Wednesday. My recommendation would be to check spotwx.com on Sunday night or Monday morning for the most up-to-date model runs.

Avalanche Summary

No new avalanches have been observed. Looking forward, new wind slab activity is expected in higher elevation lee terrain over the next few days. The expected size and distribution of new wind slab avalanches is really tough to pin down at this point due to uncertainty in the weather forecast.

Snowpack Summary

The last few days of clear skies, solar radiation, and warm air trapped at higher elevations have promoted settlement in the snowpack, and have helped to strengthen many near-surface instabilities. More recent cooling has formed a melt-freeze crust on steep solar aspects. Continued strong and variable winds have created a fairly widespread wind effect in exposed alpine terrain, and lingering wind slabs may remain reactive to the weight of a rider on isolated slopes. In more sheltered terrain a new layer of well-developed surface hoar has also developed. The mid and lower snowpack are generally strong and well-settled.

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