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Avalanche Forecast

Archived

Nov 15th, 2011–Nov 16th, 2011

Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.

Regions

Sea To Sky.

This bulletin is based on limited data. Local variation in conditions and danger levels are likely to exist. To produce more accurate forecasts, we need information. Please send an email to [email protected].

Confidence

Poor - Due to limited field observationsfor the entire period

Weather Forecast

Wednesday: 10-20cm of snow expected, with freezing levels around 900m, and moderate to strong southerly winds.Thursday: Another 5-10cm with freezing levels around 500m, and light to moderate southwesterly winds. Friday: Another pulse of significant precipitation is possible, but the timing and track are uncertain.

Avalanche Summary

No reports of avalanches, but I suspect wind slabs and any new storm slabs will be susceptible to human triggering. The size of the ensuing avalanche depends on slab thickness, with slabs thicker than 30cm generally producing avalanches sufficiently large to bury or injure a person.

Snowpack Summary

Total snowpack depth at treeline is around 60-80 cm, while many alpine areas have over a metre. Expect to find deeper pockets of wind-blown snow immediately down-wind of terrain features and ridge crests. Cold temperatures early last week resulted in some faceting, which kept surface snow cohesionless and weakened the bond to a mid-pack rain crust. However, warmer temperatures last Thursday probably helped things settle and strengthen, and may have even resulted in another crust on the snow surface, which would have been buried over the weekend.

Problems

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.