Regions
Northwest Coastal.
Spring conditions. While the freezing level remains high, wet slabs will be the primary concern.
Weather Forecast
On Saturday, light snow is forecast above about 1600 m, with light to moderate SW winds. A cold front arriving on Sunday brings 10-20 cm snow, with the freezing level falling to around 1100 m by afternoon. Clouds and a few showers may linger on Monday morning, before skies start to clear.
Avalanche Summary
There are not many commercial operations still working in the field, so information is sparse at this time of year. If you have observations from your travels, please consider sharing through the MIN (Mountain Information Network).
Snowpack Summary
As temperatures gradually cool through the weekend, loose wet and wet slab avalanches will become less likely. Storm slabs may develop in the alpine as the cold front passes through. At lower elevations, monitor the overnight freeze of the snow surface. If the snow surface does not freeze overnight or if the crust is only a few cm thick, the effect of daytime heating or rain will weaken the snowpack much more quickly than it would if there is a well frozen thick crust. Low elevation and thin snowpack areas are likely to be isothermal.
Problems
Wet Slabs
Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.
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.