Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.
Regions
Kootenay Boundary.
Bust out the sunglasses for another warm and sunny day. Warmth can weaken the snowpack quickly, so watch your exposure to steep, sunny slopes and cornices.
Confidence
Moderate - Freezing levels are uncertain
Weather Forecast
MONDAY: Sunny and warm. Freezing level near 2200 m, with cooler air in the valleys. Alpine high near +5. Light winds. TUESDAY: Sunny and warm. Freezing level near 1700 m. Alpine high near 0. Light winds. WEDNESDAY: Mix of sun and cloud. Freezing level near 800 m. Alpine high near -3. Light winds. More details can be found in the Mountain Weather Forecast.
Avalanche Summary
There were several size 1-1.5 loose wet avalanches on sunny slopes on Saturday.A wind-loaded NW slope was triggered remotely by skiers on Copper Mountain on Friday. The avalanche was reported to have failed on a layer of surface hoar. See the MIN report here.
Snowpack Summary
Warming has promoted settlement of upper snowpack layers and created surface crusts. Wind slabs exist in alpine areas and may overlie buried surface hoar. Professionals continue to monitor a couple of persistent weak layers in the upper 50-150 cm of the snowpack. Poor overnight freezes and daytime warming will keep the chance of triggering a deeper slab elevated for another day or two. Persistent weak layers are most likely to be triggered from thin, rocky areas with a variable snowpack or with a large load, like cornice fall.
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.