This forecast is based on less than 10cm of new snow Thursday night and Friday. If snow totals unexpectedly reach 15 to 20 cm, the new slab will likely be touchy, and the danger considerable at all elevations.
Confidence
Poor - Timing, track, or intensity of incoming weather system is uncertain on Friday
Weather Forecast
Synopsis: The front and the associated upper trough move through the coast Thursday night. Onshore flows in the wake of the front aren't expected to deliver more than trace amounts Friday. The story is the same though the weekend, small amounts of precipitation accompanied by moderate winds. Looks like potential for a big warm up Monday.Thursday Night: Precipitation: 3:8mm - 4:15cmFriday: Freezing Level: 1000m - 1800m; Precipitation: 1:3mm - 1:5cm; Wind: Treeline: Moderate, SW | Ridgetop: Strong, SWSaturday: Freezing Level: 1200m - 1800m; Precipitation: 1:8mm - 1:10cm; Wind: Treeline: Moderate, SW | Ridgetop: Strong, SWSunday: Freezing Level: 1200m - 1900m; Precipitation: Trace; Wind: Treeline: Light, Variable | Ridgetop: Moderate, NW
Avalanche Summary
Cornice fall on a steep north facing features at 2300m initiated a size 3 avalanche Wednesday. This likely ran on the early March melt-freeze crust. Small soft wind slabs immediately lee of ridge crest were easily managed by skiers.In the neighboring Sea to Sky region warming temps induced cornice fall Tuesday. A notable event occurred on a NE facing slope at 2100m when a falling chunk of cornice triggered a small slab immediately below the ridge. The avalanche in motion stepped down to what was likely the late March crust resulting in a size 2.5 avalanche.
Snowpack Summary
The snow surface is a mix of surface hoar, small grained facets and melt freeze crusts.Recent warm temperatures have helped to settle and strengthen the upper snowpack. Down 30 - 50 cm below the surface, snowpack tests are still producing hard resistant planar shears on the late March crust.The persistent weak layers from early March and early February continue to be a concern. The March melt-freeze crust/surface hoar is reported to be down 60 - 100cm. The February crust/facet/surface hoar layer is now deeply buried down 150 - 250cm.The lower snowpack is strong and well settled.
Problems
Storm Slabs
Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.