Boletín de aludes

Purcells

Nov 24 – 25, 2015Avalanche Canada
Ver en el mapa
Archivado · caducó 11 years ago

Peligro de aludes

Thu
Fri
Alta montaña
Sin grado
Límite del bosque
Sin grado
Bajo el límite
Sin grado
Abrir el mapa completo

Lo esencial

This forecast is based off a pretty meager set of observations. If you're out, please let us know what you're seeing via the Mountain Information Network. MIN

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible - Likely
    Tamaño
    1–3
    Winds out of the north are likely driving wind slab formation on southerly features. These slabs are probably most problematic immediately lee of ridge crest, but you may encounter them in the right feature at treeline too.

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely
    Tamaño
    4–6
    While many of our November wear layers are becoming less reactive, it's important to remember that there may be a weak layer of crust and facets near the ground. This is probably only a concern on north through east facing alpine features.

Weather Forecast

Arctic air slides down from the north resulting in clear skies and cooler than average temperatures for the forecast period. Strong N/NE winds at ridgetop are expected to continue through Wednesday afternoon, and then back off to light northerly for Thursday and Friday. We may see above freezing temperatures in the alpine beginning Friday evening, time will tell what the extent of this will be. No significant precipitation/snowfall expected for the forecast period. For a more detailed mountain weather forecast visit avalanche.ca/weather

Avalanche Summary

Control work in the north of the region Tuesday produced wind slabs to size 1 on high elevation south facing features.  No other recent avalanche activity has been reported.

Snowpack Summary

Monday's storm snow fell on a variety of old surfaces including crust, surface hoar and old settled snow. Arctic air moving into the region has resulted in northerly winds which have formed small wind slabs on south facing features near ridge top. Warm temps and strong solar input formed a crust on south facing features which can be found underneath Monday's storm snow. There are at least three surface hoar layers in the snowpack buried on: Nov. 5th, Nov. 11th and Nov. 23rd. The first two have been largely unreactive. Facets may exist just above the ground on shaded slopes in the alpine.

Regiones cubiertas