Up to 20cm of new snow has been forecast over the next 24 hours. There will be good skiing in sheltered treeline locations.
Weather Forecast
Starting this evening light rainfall will transition into snow. Amounts will be greatest at upper elevations where over the next 24 hours 20cm may fall. Winds will be light out of the NE at lower elevations and moderate SW near ridge tops gusting strong. The overnight temperatures may not allow for good crust formation at mid treeline elevations.
Snowpack Summary
Below Treeline a supportive 15cm melt freeze crust provides temporary stability above a wet and unconsolidated snowpack. The crust thins with elevation and on slopes which are not South facing. By mid afternoon, or earlier on very hot days, this crust will melt and the avalanche danger will elevate considerably. The base of the snowpack is weak.
Avalanche Summary
Evening rain may see a short lived spike in wet avalanches at lower elevations this evening. The falling temperatures will put a stop to this as the rain transitions to snow. Ridge top winds will produce soft slabs with the new snow and where this happens to fall on an established melt freeze crust bonding will likely be poor, at least initially.
Confidence
Track of incoming weather systems is uncertain
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.
Cornices
Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.