Avalanche Forecast

High

A dry ridge of high pressure will develop over the region bringing clear skies for Thursday and Friday. Increased cloud is forecast for Saturday. Ridgetop winds will be light to moderate from the northwest on Thursday morning, and then become light for the rest of the forecast period. Freezing levels will hover around 1200m on Thursday, 1500m on Friday and 2100m on Saturday.

On Tuesday, several natural or human triggered wind slabs to size 2.5 were observed on a variety of aspects at treeline and in the alpine. Persistent slab avalanches continue to fail on the late February weak layer. A sledder was killed on Sunday in a size 2 slab avalanche in the Monashees just north of Shuswap Lake. The avalanche occurred on a west facing convex roll at 1830m. The slab was 40-80cm deep, 60m wide and 65m long. The subject was found after more than an hour of probing as rescuers were not able to obtain a transceiver signal. Although this avalanche occurred only a few kilometers north of the regional boundary in the North Columbia region, similar conditions exist in the South Columbias. This was indicated by another avalanche in the southeast corner of the region (see the Mountain Information Network post near Kokanee Glacier). The avalanche, which resulted in a partial burial, was remotely triggered and was in the size 2 range. As stormy weather tapers-off and a dry ridge builds over the province, solar radiation will become the driver for natural avalanche activity.

On lee features at treeline and in the alpine light amounts of new snow overlie older wind slabs while intermittent sunny skies have promoted a melt-freeze cycle on some sun-exposed slopes. 60-110cm below the surface you'll find a persistent weak layer comprised of surface hoar, facets and/or a thick crust. This layer, which was buried on February 27th, seems variably reactive. In other words, it's still touchy in some places while in other places it's really tough to trigger, and there's not much of a reliable pattern telling us what exact aspects are most suspect. I'd continue to be suspicious of steep, unsupported features at treeline and in the alpine as this layer has the potential for very large avalanches. Below this interface, the snowpack is generally gaining strength. At ridgetop, cornices are huge and could be become increasingly touchy with forecast solar radiation.