Avalanche Forecast
Issued: Apr 7th, 2014 10:33AM
The alpine rating is Deep Persistent Slabs, Wet Slabs and Wind Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Fair - Freezing levels are uncertain on Monday
Weather Forecast
Synopsis: The ridging is looking a bit weaker today, but the freezing level is still forecast to top out around 2300m Monday, and its expected to remain there through Tuesday afternoon. The warming will likely be most pronounced in the southern half of the region.Monday Night: Freezing Level: 2300m - 2500mTuesday: Freezing Level: 2300m - 2500m; Precipitation: Trace; Wind: Treeline: Moderate, SW | Ridgetop: Strong, SWTuesday Night: Freezing Level: 2500m lowering to 1300m; Precipitation: 4:8mm - 4:15cm;Wednesday: Freezing Level: 1200m - 1800m; Precipitation: Trace; Wind: Treeline: Light, W | Ridgetop: Moderate, WThursday: Freezing Level: 1200m rising to 2200m; Precipitation: Nil; Wind: Treeline: Light, Variable | Ridgetop: Moderate, W
Avalanche Summary
On Saturday night a natural avalanche started on a steep southeast facing alpine feature and eventually stepped down to ground resulting in a size 4 avalanche in the central portion of the region. The avalanche was estimated to be 1000m long, 600m wide, and up to 300cm in depth.
Snowpack Summary
Recent warm temperatures have resulted in good settlement and bonding of the storm snow from last week, but there are still isolated rider triggerable wind slabs on wind exposed alpine features.Three persistent weak layers exist in the highly variable snowpack of the Columbias:The mid-March sun crust/surface hoar layer down 50-80cm still has potential for human-triggering in isolated areas. The early-March crust/facet/surface hoar layer down around 80-120cm has become less susceptible to human triggering, but still has the capacity to produce large avalanches.The mid-February crust/facet/surface hoar combo is typically down 60 - 120cm. Direct triggering of this layer has become unlikely, however, cornice fall, a smaller avalanche in motion or prolonged warming may wake this layer up, which would result in very large and destructive avalanches.Weak basal facets exist in many areas, but triggering is unlikely.
Problems
Deep Persistent Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Wet Slabs
Aspects: All aspects.
Elevations: All elevations.
Likelihood
Expected Size
Wind Slabs
Aspects: North, North East, East, South East, South, South West.
Elevations: Alpine.
Likelihood
Expected Size
Valid until: Apr 8th, 2014 2:00PM