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Avalanche Forecast

Feb 4th, 2014–Feb 5th, 2014
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
2: Moderate
The avalanche danger rating in the alpine will be moderate
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low
Alpine
1: Low
The avalanche danger rating in the alpine will be low
Treeline
1: Low
The avalanche danger rating at treeline will be low
Below Treeline
1: Low
The avalanche danger rating below treeline will be low

Regions: South Columbia.

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Confidence

Fair - Wind effect is extremely variable

Weather Forecast

Synopsis:  A very strong ridge of high pressure continues to dominate the weather pattern.  In the extended period the models are not breaking down the ridge as quickly, so it looks like Saturday will be dry throughout the province.Wednesday: Sky: Clear; Freezing Level: Valley Bottom; Precip: Nil Wind: Light, NE | Mod, NE at ridgetop.Thursday: Sky: Clear; Freezing Level: Valley Bottom; Precip: Nil Wind: Light, NE Friday: Sky: Clear; Freezing Level: Valley Bottom; Precip: Nil Wind: Light, NE

Avalanche Summary

Fast moving loose dry avalanches and small wind slabs continued to be sensitive to human triggering Monday.Deep Persistent Slabs have been removed from the problem portion of the forecast because it's probably a 1:1000 slope event at this time, but they haven't totally gone away. Two large natural avalanches (size3) were observed on a steep south facing alpine feature south of Revelstoke on Saturday.

Snowpack Summary

Snow totals from the last pulse on Wednesday (140129) range from 5 - 20 cm with the greatest accumulations in the south of the region. This snow is faceting quickly in the cold temps. In wind exposed terrain, especially in the alpine, winds continue to form shallow wind slabs that are most prevalent immediately lee of ridgecrest.  These variable wind slabs should stick around a bit longer than we're accustomed to as they are resting on a weak layer composed of large grained surface hoar (widespread in most sheltered and shaded areas at all elevations), a sun crust on open south facing slopes, faceted grains (in colder areas or areas with a thinner snowpack), or a combination of the above.Most of the snowpack is generally well consolidated. However, in thinner snowpack areas a facet/crust weakness may exist near the bottom of the snowpack. The depth of this layer makes human triggering unlikely, but the consequences of doing so could be disastrous.

Avalanche Problems

Wind Slabs

Erratic winds have formed thin wind slabs that are most prevalent immediately lee of ridgecrest.  Spirited sluffing and touchy wind slabs should stick around a bit longer than usual due to the variety of persistent weaknesses buried beneath them.
Highmark or enter your line well below ridge crests to avoid wind loaded pillows.>Carefully consider the impact a thin wind slab will have on your proposed line, especially in high consequence terrain. Have a backup line in mind in case you need to seek more sheltered riding. >On steep slopes, pull over periodically or cut into a new line to manage sluffing.>Watch for terrain traps where small amounts of snow will acumulate into deep deposits.>

Aspects: All aspects.

Elevations: Alpine.

Likelihood: Possible

Expected Size: 1 - 3