Regions
Northwest Inland.
Confidence
Fair - Timing or intensity of solar radiation is uncertain on Tuesday
Weather Forecast
Tuesday: Very light snowfall with a mix of sun and cloud / Moderate west winds / Freezing level at 800mWednesday: Generally clear in the morning with increasing cloud throughout the day / Light northwest winds / Freezing level at 1200mThursday: Light to moderate snowfall / Moderate west winds / Freezing level at 1200m
Avalanche Summary
Numerous loose wet avalanches have occurred from steeper solar aspects up to size 2.0. Large cornice releases have also been noted.
Snowpack Summary
Surface snow has settled with the influence of warm temperatures and surface faceting continues on steep shaded alpine slopes. Solar aspects at all elevations and all lower elevation terrain are now well into a daily melt-freeze cycle with sun-exposed slopes becoming very weak with daytime warming. 30 - 60 cm of snow overlies a crust, old wind slabs or surface hoar layer buried on March 9th. The distribution of the surface hoar is also highly variable and it does not exist in every drainage. I would still remain conservative and continue to dig and test before diving into my line. Deeper in the snowpack, basal facets may resurface as a concern with forecast warming.Cornices have become well-developed and could easily become unstable during periods of warm weather or direct solar radiation.
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.
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.