Confidence
Fair - Freezing levels are uncertain
Weather Forecast
Overnight and Wednesday: A mix of snow, rain, and strong Southwest winds is expected overnight as a cold front moves across the region. The freezing level will drop from 2800 metres down to 1500 metres during the light precipitation. Mostly clear skies during the day with light winds and freezing level rising to 2000 metres.Thursday: Mostly sunny with light winds and freezing levels rising to 2300 metres.Friday: Overcast with moderate Southwest winds and light precipitation starting in the afternoon.
Avalanche Summary
A size 3.0 avalanche in the Harvey pass area was reported to have started from a cornice fall and stepped down to the February deep persistent weak layer. Avalanches sliding on this layer are expected to become less likely with the forecast cooler temperatures and lower freezing levels.
Snowpack Summary
Very warm temperatures over the past few days and high freezing levels with no crust recovery have resulted in moist or wet snow at all elevations.In the Smith Basin area there is 140 cm below treeline and the top 40 cm was found to be moist and well consolidated. The March crust below was decomposing at this location. The February deep persistent weak layer was down 80 cm and well preserved. Higher up at about 2300 metres the height of snow was a little over two metres. The March crust was not intact at this location and did not result in any shears in snow profile tests. The February deep persistent weak layer (DPWL) was down 100 cm and was a well defined layer of softer facetted snow below the hard (pencil) snow of the well settled mid-pack. Hard sudden collapse shears were recorded at the interface of the February DPWL. In the Elk Valley South the height of snow at 1900 metres was 430 cm. The snow was dry and loose above 1700-1800 metres and moist below where loose wet slides had released on solar aspects. There was a 2-3 cm supportive crust on Southerly aspects above 1900 metres, and no crust on shaded North aspects.
Problems
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.
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.