Boletín de aludes

South Coast

Jan 20 – 21, 2016Avalanche Canada
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Archivado · caducó 11 years ago

Peligro de aludes

Fri
Sat
Alta montaña
4 · Fuerte
Límite del bosque
4 · Fuerte
Bajo el límite
4 · Fuerte
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Lo esencial

Conditions are ripe for an impressive avalanche cycle. Thursday is a day to wait out the storm from a safe place.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Very Likely
    Tamaño
    2–5
    Expect heavy loading from snow, rain, and wind to overload buried surface hoar, potentially creating very large avalanches. This problem has been most active on shady slopes near treeline.

  • Storm Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Likely - Very Likely
    Tamaño
    1–4
    Expect new touchy storm slabs to form with heavy loading from snow and wind on Thursday. Widespread loose wet sluffing in steep terrain below treeline is also likely.

Confidence

High

Weather Forecast

Tonight and Thursday: 30-50 cm of snow. The freezing level starts near 1000 m and rises to 1600-2000 m late in the day. Winds are strong from the South. Friday: A few flurries and a clearing trend. The freezing level dips slightly to 1500 m. Winds ease to light from the SW. Saturday: Cloudy with sunny breaks. The freezing level is around 1200 m and winds remain light from the W-SW.

Avalanche Summary

A fairly widespread natural avalanche cycle was reported below treeline on Tuesday. Numerous slab avalanches up to size 2 were observed, primarily on sun affected slopes. On Tuesday there was also an incident on Mount Chief Pascal. One person was partially buried after triggered a 60-80 cm deep slab on North aspect near treeline. Check the Mountain Information Network for photos and more information on this incident. Conditions are primed for a large and widespread natural avalanche cycle with the incoming storm on Thursday.

Snowpack Summary

30-40cm of fresh storm snow has buried the recently formed mid-January surface hoar layer. Below that are the two early-January interfaces down 50-80cm which are separated by around 5-10cm of snow and both consist of a sun crust on steep solar aspects and a layer of surface hoar on sheltered and shady slopes. Strong southeast through southwest winds have been loading lee features at treeline and in the alpine. The mid and lower snowpack is generally strong, with the exception of shallow snowpack areas that may be more faceted.

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