Conditions are improving but continue to exercise caution in wind affected terrain and during periods of intense sunshine.
Weather Forecast
Synopsis: A building ridge of high pressure should give the South Coast dry conditions with a mix of sun and cloud for the next few days. The freezing level is around 1000 m on Tuesday but could bump up to 1800-2000 m on Wednesday/Thursday. Ridge winds should be light and variable. The next significant weather system might reach our region on Friday bringing moderate snow or rain.
Avalanche Summary
Several size 2 natural wind slabs were observed throughout the region on the weekend. The storm slab was reported to be sensitive to rider triggered at and below treeline in the Northern part of the region on Sunday. Here it was failing on the crust/surface hoar interface down around 35 cm.
Snowpack Summary
Recent snowfall amounts vary from north to south with an average of 25-35 cm of new snow near the Duffey Lake Road and 40-60 cm in the Cascades (Coquihalla and Allison Pass). Strong W-SW winds have formed deep and dense wind slabs in wind-affected terrain. The fresh storm and wind slabs overlie a hard crust and/or surface hoar. Recent snowpack tests show the potential for riders to trigger avalanches at this interface below the storm snow. Deeper snowpack weaknesses are still on our radar, but seem to be dormant for the time being.
Problems
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.
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.