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Avalanche Forecast

Archived

Nov 30th, 2013–Dec 1st, 2013

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

Regions

South Rockies.

New snow and wind will start to develop storm slabs. Recently buried surface forms may not bond well to the new snow.

Confidence

Poor - Timing, track, or intensity of incoming weather system is uncertain

Weather Forecast

Overnight and Sunday: Light snow in the morning but picking up in the evening with an associated increase in westerly winds. Expect 5-10cm and moderate to strong westerly winds by the end of the day. Freezing levels should remain in valley bottoms.Monday: Continued moderate to locally heavy snowfall with the heaviest amounts likely on the east of the divide. Strong winds shifting to north-easterly as the temperatures drops.Tuesday: Becoming clear and cold with North-easterly winds.

Avalanche Summary

Smooth alpine slopes that did not previously slide may still be of concern. With very little data on the current conditions, you need to be your own detective out there. If you see or trigger an avalanche, please send us a note at: [email protected].

Snowpack Summary

Treeline snowpack depths in sheltered areas vary between approximately 40-100 cm. The current snowpack has been subjected to strong wind, cold temperatures and chinook driven warming. As a result it should be easy to find wind scoured snow, old wind slabs, crusts and faceted snow. Crusts with associated facets may be lurking near the base. This weakness may still be of concern on isolated smooth terrain features that have not seen avalanche activity.

Problems

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.