Regions
Northwest Inland.
When the sun comes out on Wednesday, expect lots of solar triggered sluffing on steep slopes. Thin new wind slabs may be reactive in leeward features in the alpine.
Weather Forecast
A mix of sun and cloud is expected for Wednesday and Thursday with light southerly winds in the alpine and afternoon freezing levels around 1500-1600m. Mainly cloudy conditions are expected for Friday with the possibility of light showers. Alpine winds are forecast to be moderate from the southwest with afternoon freezing levels around 1500m.
Avalanche Summary
On both Sunday and Monday, loose wet avalanches up to size 2.5 were reported in the far north of the region. With the arrival of spring, field observations and data have become very limited in the region. A lack of avalanche reports does not mean avalanches are not occurring. On Wednesday, newly formed wind slabs are expected to be reactive to human-triggering in the alpine. Widespread solar triggered loose sluffing is expected with the new snow sliding on the firm crust layer. Cornices have been weak recently and may fail naturally with storm loading.
Snowpack Summary
The new snowfall will bury a widespread melt-freeze crust. Strong southerly winds in the alpine will have likely formed thin wind slabs. The region should return to melt-freeze conditions on Wednesday with surface crusts forming overnight and breaking down during the day. The snowpack's strength is directly related to the thickness and strength of these surface crusts. A widespread crust/facet layer from early February and depth hoar at the bottom of the snowpack are dormant. Cycles of melting and refreezing have limited the reactivity of these old layers. However these layers, or the ground, could potentially once again be the layer for an isolated yet large avalanche with prolonged periods of warming.
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.
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.