Stay alert to conditions that change with aspect, elevation and time of day. Watch for clues like a moist or wet snow surface that indicate its time to find colder snow or head for home.
Weather Forecast
WEDNESDAY: Freezing level starting at 1000m, rising to 2000m. Light N/NE winds at all elevations. No significant precipitation expected. Clear skies initially, cloud cover building in the afternoon.THURSDAY: Freezing level starting near 1500m, rising to around 2200m. Light W/SW winds at all elevations. Clear skies. No significant precipitation expected.FRIDAY: Freezing level starting at 1500m rising to 2200m. Light SW winds at treeline, moderate SW winds at ridgetop. No significant precipitation.
Avalanche Summary
Several cornice falls have been reported in the last few days, some of which have triggered avalanches on slopes below.
Snowpack Summary
The recent 10 to 25cm of storm snow was shifted by variable strong winds into wind slabs on lee slopes above 2000m. These wind slabs are probably growing old and tired. Cornices are large and touchy in some spots. The new snow sits over a crust which is generally becoming more supportive. Low elevations sport an isothermal snowpack, which is now capped by a refrozen crust.Persistent weak layers in the upper snowpack remain a lingering concern, although they seem to be slowly gaining strength. In the north of the region, the mid-March crust/facet layer is down 40-60cm. The mid-February crust/facet/surface hoar layer, down about 80 cm, may also still be reactive in isolated areas. Weak layers which formed earlier in the winter are also a concern in certain spots. Look for a revised snowpack description tomorrow. (April 8th)
Problems
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.