Confidence
Fair - Due to variable snowpack conditions on Saturday
Weather Forecast
Overnight and Saturday: A ridge of High pressure will build over the North Coast tonight and then move down onto the South Coast during the morning. Light snow is expected to bring a couple of cms to the region during the evening. Moderate Northwesterly winds and cooling temperatures (-12.0 in the alpine) are forecast by morning. Broken skies in the morning, with some sunny periods in the afternoon.Sunday: A warm front is expected to sweep across the coast on Sunday. Expect light to moderate westerly winds combined with moderate precipitation. Freezing levels should gradually rise up to about 1200 metres.Monday: Light precipitation and moderate westerly winds combined with freezing levels rising during the day to about 1000 metres.
Avalanche Summary
We have a report from Thursday of a small size 1.0 skier/rider accidental triggered avalanche on a NE aspect at 1900 metres that released in the new snow. There have been no new avalanches reported releasing on the November rain crust.
Snowpack Summary
The recent very strong wind event has caused extensive wind scouring in the alpine and at treeline. Ski penetration is limited to about 15-20 cm above a stiff buried wind slab. Foot penetration may still be up to 70 cms as the wind slab is not able to carry the weight of a person without skis. The recent storm snow (up to about 130 cms) appears to be bridging above the early November weak layer, and we are not seeing deep releases down to the rain/ice crust. There is not much discussion about surface hoar that was buried last week, and we are not getting reports about test results on that layer. Professionals are concerned about the early November rain crust. If this deep persistent weak layer (DPWL) becomes reactive, the consequences will be very large destructive avalanches. The crust may be buried between 100-200 cms depending on the total depth of the snowpack in your area. The crust may be a bigger problem where it has a layer of facetted crystals above, rather than where it is like a laminated sandwich of crusts and facets. If that sounds too technical for you, then the take home is that this is not an easy problem to gauge when or where it might wake up.
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.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.