Boletín de aludes

Kananaskis

Feb 23 – 24, 2015Alberta Parks
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Archivado · caducó 12 years ago

Peligro de aludes

Wed
Thu
Alta montaña
2 · Moderado
Límite del bosque
2 · Moderado
Bajo el límite
1 · Débil
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Lo esencial

High northern aspects are the place to look for good snow at this point.

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–2
    These slabs area relatively easy to spot and predict. Open slopes at treeline is where these slabs start to appear.

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    1–3
    The post Jan 31st slabs have been reclassified as a persistent problem. Steep areas below ridge crests are a likely place to encounter this issue. The slabs are generally thick, and hard. Its unlikely to hit one, but it will be big if it happens.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    3–5
    As our snowpack slowly grows it becomes easy to forget about the bottom layers. Remember that the bottom is still weak in many places and requires a deep snowpack to safely bridge the bottom layers.

Confidence

Good

Weather Forecast

A cloudy day tomorrow should keep the solar aspects a bit cooler than today. An overnight low of -9 will refreeze today's suncrust. The alpine high will hit -4. Ridge winds will be light, and gusting to moderate from the west. Freezing level is expected to be 1700m. No precip is expected.

Avalanche Summary

A few isolated loose wet avalanches were noted today. All were about sz1.

Snowpack Summary

Valley bottom up to 2100 is still suffering from the Feb crust. There is 5-10cm's on top of it which is making upward travel easier . On the way down , the crust is breakable in many places and tricky skiing. At treeline the crust almost instantly turns to hard slab. These slabs were formed by a wind event last week. The density of these slabs ranges from very hard (hard to get an edge) to breakable. Beneath these new slabs are the older Jan 31st slabs, down 30-50cm's. The alpine has had considerable wind over the past week. In places the underlying layers have been blown clean. The windloading pattern is very easy to see right now. At all elevations, the sun had a huge impact today. A sun crust will be present on all south aspects and its thought to extend up to 2500m.

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