Regions
Northwest Coastal.
If you're heading to the north of the region, the snowpack changes. See the Forecast Details page for more info.
Confidence
Fair - Timing or intensity of solar radiation is uncertain
Weather Forecast
Expect a mix of sun and cloud for the forecast period with light flurries possible on Monday evening. Winds should remain generally light with daytime freezing levels sitting at about 1500m.
Avalanche Summary
On Friday, explosives control triggered wind slab avalanches to size 2 in the north of the region.No other recent avalanches were reported. With sunny breaks forecast for the next few days loose wet avalanches are possible in sun-exposed terrain.
Snowpack Summary
Smaller wind slabs have formed in high elevation lee terrain. These wind slabs overlie a variety of surfaces which include older wind slabs or melt-freeze crusts. Up to a metre below the surface you may find a hard crust which co-exists with facets, especially in the north of the region. Although reports suggest this layer has gained strength, I'd be wary of the possibility of isolated large avalanches on steep, unsupported slopes, especially if temperatures increase, or if solar radiation is strong. The mid-pack is generally well-settled and strong. At the base of the snowpack, weak facets may be found, particularly on shallow alpine slopes in the north of the region. Cornices are large and potentially fragile. Below treeline, the snow appears to be in a spring melt-freeze cycle.
Problems
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.
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.