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Avalanche Forecast

Archived

Dec 7th, 2011–Dec 8th, 2011

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

Regions

Kootenay Boundary.

Confidence

Good - -1

Weather Forecast

A ridge of high pressure builds back into the area Thursday and then dominates the weather pattern through the end of the work week. Winds will be at light to moderate speeds out of the NW all day Thursday under bluebird skies. Freezing levels creep up to 900m before dropping back to the valley floor overnight. Temps are cool; I'm expecting daytime highs near -4 at treeline Thursday with overnight low's dipping down to -12. Friday looks to be more of the same.

Avalanche Summary

No recent avalanche activity has been reported. If you have any avalanche observations to report, please email us at: [email protected].

Snowpack Summary

Some great observations have come our way recently. While there are a few players in the snowpack, none of them seem to be doing anything at the moment. A rain crust is present just below the snow surface below 1800m. The crust, in combination with cool temperatures, has really settled things out at & below treeline. My main concern is the odd lingering windslab still scratching out a living in the alpine. But, I know that this is less & less of an issue every day. I'm thinking about bringing the Alpine Danger down to Low for the weekend. In order to feel comfortable with that I need some more feedback/observations. If you're out & about please drop me a line & let me know what you're seeing: [email protected] snowpack sounds pretty well organized at the moment. A bit of soft fist snow can be found in upper elevations with a good tight midpack consisting of more dense snow below. The alpine is holding 150-200cm. Treeline depths are between 50 -150cm. Recent snowpack observations indicate that the late October rain crust is present in the alpine elevations and down approximately 120cm. This crust is said to be up to 5mm in thickness with faceting below it. For the moment the crust seems to be bridging over the facets below, with a well settled 1F - P midpack above.

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.