Boletín de aludes

Kananaskis

Nov 8 – 9, 2018Alberta Parks
Ver en el mapa
Archivado · caducó 8 years ago

Peligro de aludes

Sat
Sun
Alta montaña
2 · Moderado
Límite del bosque
1 · Débil
Bajo el límite
Sin grado

Lo esencial

We spotted a healthy sz 2.5 on Tent Ridge during our drive today. While Tent Ridge is a known performer, it is very unusual to have an avalanche of this size so early in the season. Be very cautious on, or near slopes that have the Oct 26 crust.

Problemas de aludes

  • Deep Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely - Possible
    Tamaño
    1.5–3
    Deep persistent layer?? Already? Yes. This only means the trouble layer is near the bottom of the snowpack. The "deep" part is a bit of a misnomer in these parts. This layer is widespread in the alpine, but becomes more spotty at lower elevations.

Confidence

Moderate - Due to the number and quality of field observations

Weather Forecast

Temps will be steady around -10 tomorrow with some light cloud cover and flurries starting mid morning. Amounts won't add up to anything significant. Winds will be light from the west.

Avalanche Summary

The east face of Tent Ridge avalanched sometime within the last 12hours (as of 11am this morning). It was a healthy sz2.5, possibly even a sz3. The debris wasn't visible to confirm. It looked like a cornice and/or rapid warming trigger and appeared to fail on the Oct 26 crust. East aspect and wind loaded from an earlier wind event.

Snowpack Summary

The distribution of snow still varies throughout the range, but in alpine areas along the Spray Range, there is enough snow to make avalanches an issue. Highwood Pass is a bit further behind, but there are certainly areas there that also have enough snow. The alpine snowpack is made up of a few significant layers: The basal layers, the Oct 26 crust, and the surface slabs. The basal layers are already facets and some depth hoar in shallow areas. The Oct 26th crust is an unwanted "gift" from the early September snowstorm. Direct observations are limited, but it seems the crust is intact with facets above and below. This Deep Persistent layer will be the one to watch for some time. It is buried anywhere between 20cm and 80cm in blown in areas. In some areas, there is also a second crust that has been reported.

Regiones cubiertas