Avalanche Forecast

Low - Due to the number of field observations

We're looking at cool temperatures and some gusty west through north winds for the next few days. Overnight lows will be near -20 Celsius at tree line. TUESDAY: A mix of sun and cloud. Ridge wind becoming strong from the west. Temperature -7. Freezing level 1100m in the afternoon.WEDNESDAY: Flurries (5 -15cm accumulation). Ridge wind moderate gusting strong from the north / east. Temperature -7. Freezing level valley bottom.THURSDAY: Sunny with cloudy periods. Ridge wind gusting moderate from the west. Temperature -10. Freezing level valley bottom.

A widespread natural avalanche cycle occurred Thursday afternoon and overnight into Friday. Several storm slabs and deep persistent slabs to size 4 were reported when visibility improved on Friday. See this MIN post for more information. These avalanches are failing on weak layers deep in the snowpack and running to valley bottoms. See this video for more details. On Wednesday, naturally triggered deep persistent slab avalanches up to size 2.5 were reported in the Alexander Creek Drainage. The suspected failure layers were mid-December or late-November layers near the base of the snowpack. Also avalanche control in the Line Creek area produced several size 2.5 and two size 3 avalanches that also failed on weak layers near the base of the snowpack. A week ago in the neighboring Lizard Range, the east facing Mt Corrigan slide path produced a very large natural avalanche estimated to be a size 4.0, which took out mature timber in the path as it overran the Flathead FSR south of Corbin.

Temperatures cooled to -20 overnight at tree line and winds have been gusty (mostly north west to south west) throughout the weekend. Storm snow totals from last week were 50-90 cm, and redistributed by winds (see above) at higher elevations. The western parts of the region in BC were relatively warm with less snow, while areas in Alberta and around the divide were much colder and windier. The lower snowpack in this region is weak, with two main concerns: A widespread weak layer from mid-December composed of facets, crusts, and surface hoar is 100-150 cm deep. Second, a rain crust with sugary facets buried in late-November is near the bottom of the snowpack. Although the snowpack structure is variable across the region, these persistent weak layers are generally widespread.The take home message is that weak layers are still active and deserve a lot of respect. The solution is to stick to conservative terrain while avoiding all overhead hazard.