Avalanche Forecast
Issued: Dec 12th, 2015 8:41AM
The alpine rating is Storm Slabs and Persistent Slabs.
, the treeline rating is , and the below treeline rating is Known problems includeSummary
Confidence
Low - Timing, track, or intensity of incoming weather system is uncertain on Sunday
Weather Forecast
A tightly wound and rapidly deepening low pressure centre is expected to track just south of Vancouver Island Saturday afternoon. The northern edge of this system should track through the Purcells Saturday night with lingering convection generating continued snowfall through the day Sunday. A ridge is expected to take over the pattern Monday afternoon and should persist through Wednesday. SATURDAY NIGHT: 2 to 10cm of snow, freezing level near valley bottom, moderate to strong SW winds. SUNDAY: 1 to 5cm of snow, freezing level rising to 1000m, moderate to strong SW winds. MONDAY: 1 to 5cm of snow, freezing level near valley bottom, light W/NW winds. TUESDAY: No snow expected, freezing level at valley bottom, light variable winds.
Avalanche Summary
On Friday two significant observations were reported: The first was a size 3.5 natural avalanche that was observed on a SE facing feature at 2800m running to ground in some places. The second was a report of a skier triggered size 2.5 avalanche that was accidentally triggered on an east facing feature at 1500m in the northern Purcells. This avalanche failed on the early December Persistent Weak Layer. Control work in the central and southern Purcells Thursday produced avalanches to size 3.5 on a variety of aspects, some of which ran full path.
Snowpack Summary
A string of storms between December 2nd and December 11th produced 35 - 80cm of storm snow in the Purcells which is settling out at all elevations. You may find a brittle crust about 10 to 20cm below the snow surface as high as 2000m that was formed by rain and warm temperatures last Tuesday. Below all the new snow lies the early December persistent weak layer. This weak layer manifests as an old sun crust on due south facing features in the alpine, large grained surface hoar below 1800m and small facets in isolated pockets. The surface hoar is the major player and it's been most reactive below treeline between 1400 and 1800m. Recent winds out of the south and southwest have formed wind slabs on lee features that are mainly confined to the alpine, but you may find the odd fresh wind slab at treeline too. The mid and lower portions of the snowpack are thought to be well settled.
Problems
Storm Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Persistent Slabs
Aspects: All aspects.
Elevations: Alpine, Treeline.
Likelihood
Expected Size
Valid until: Dec 13th, 2015 2:00PM