Avalanche Forecast
Issued: Dec 29th, 2011 9:31AM
The alpine rating is Storm Slabs, Wind Slabs and Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Fair - Intensity of incoming weather is uncertain on Friday
Weather Forecast
Friday: Snow amounts 10-15cms. Ridgetop winds 40km/hr from the West. Freezing levels could rise to 1000m. Saturday/Sunday: A ridge of high pressure is expected to move into the region for the weekend. A mix of sun and cloud with few flurries in the West. Mainly sunny skies in the Eastern part of the region. Temperatures should remain seasonal.
Avalanche Summary
Reports of natural large avalanches to size 3 have occurred throughout the South Columbias. Continued reports of rider triggered avalanches up to size 1.5, and natural cornice failures triggering slopes below up to size 2.5. The focus is on elevations between 1300-2100m, and mainly on North-South aspects. This avalanche cycle indicates that the December 24th surface hoar and the mid-December surface hoar layers have reached the tipping point and are producing large slab avalanches. Check out the Forecasters Blog to see an updated avi picture. It clearly indicates how touchy the surface hoar layer is on convexities and low angle terrain.
Snowpack Summary
The region has received storm snow amounts up to 50cms since December 26th. Wind slabs continue to form on North-South East aspects in the alpine and exposed treeline locations. New storm snow blankets elevations above 1100m. Below is receiving rain instead of the fluffy white stuff. In the upper meter of the snowpack two different weak layers exist. From the top down approx. 30-40cms lies the December 24th surface hoar layer. It has become very reactive over the past 24hrs in most locations across the region. Field tests show easy shears on this layer and Rutchblock 3 (Whole Block) scores. This layer can be found in sheltered areas at treeline and below. Going down 70-100cms is the mid-December surface hoar layer. This layer has naturally reached its threshold in the southern part of the region. In the Northern locations this layer is very sensitive and reactive to new loading from snow, wind, rain, and/or human trigger. This surface hoar layer is still producing sudden planar results in stability tests. These are the layers to watch. Below this sits a well consolidated, strong midpack.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Wind Slabs
Aspects: North, North East, East, South East.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Valid until: Dec 30th, 2011 8:00AM