Boletín de aludes

Kananaskis

Mar 1 – 2, 2013Alberta Parks
Ver en el mapa
Archivado · caducó 14 years ago

Peligro de aludes

Sun
Mon
Alta montaña
4 · Fuerte
Límite del bosque
3 · Notable
Bajo el límite
1 · Débil
Abrir el mapa completo

Lo esencial

Tonight will bring a spike in precip, alpine winds and temperature. With that spike, a rapid deterioration in avalanche conditions can be expected. Give alpine features lots of respect tomorrow. MM

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2–4
    windslabs at treeline and above are still possible to trigger. Convex rolls in steep terrain below ridge crests and steep crossloaded gullies are particulary concerning. Expect to start finding these at the upper margin of TL.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    2–5
    Buried wind slabs (originally formed in late January) are still a concern in steep features in the alpine and at treeline. These slabs are found down 30 to 60cm in the snowpack. Additional load may make these easier to trigger.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3

Confidence

Fair - Intensity of incoming weather is uncertain on Saturday

Weather Forecast

The spring like conditions will continue for the next 24 hours. The precip associated with the Pineapple Express will peak at midnight tonight. We can expect up to 20 cms near the divide. Winds are now forecasted to be slightly less than they were, BUT this puts them in a range that is even more conducive to wind slab development.

Avalanche Summary

No new avalanche observations today due to poor visibility.

Snowpack Summary

Light precip today has left us with 10cm at TL and counting. This new snow has come in warmer than usual. Expect to see a dramatic change in snow density as you climb higher. ALP elevations will have dry snow that is more than willing to be transported by the wind. Expect storm slabs. TL has the most variable snow density. Transport will increase in proportion to the wind. BTL snow is heavy and sticky. It will bond quickly, however "upside down" conditions can be expected.

Regiones cubiertas