Purcells

New snow is on the way which is GREAT, but multiple buried weak layers in our snowpack remain capable of producing large human triggered avalanches. The message may be getting repetitive, but conservative terrain selection remains a must.

Moderate - Timing, track, or intensity of incoming weather system is uncertain on Wednesday

On Wednesday morning a strong winter storm will arrive on the BC coast. Rather warm air and precipitation is expected to spread into the interior Wednesday afternoon resulting in snowfall through Thursday evening. The freezing level should fall back towards valley bottom Thursday night. Friday and Saturday look cool and calm with another system set to move into the interior on Sunday. WEDNESDAY: Broken cloud cover, freezing level rising to around 1000 m, moderate southwest wind, trace of snow possible in the afternoon, 2 to 12 cm possible Wednesday night.THURSDAY: Broken cloud cover, freezing level around 1600 m, moderate to strong southwest wind, 1 to 8 cm of snow possible. FRIDAY: Scattered cloud cover, freezing level beginning at valley bottom rising to around 1200 m in the afternoon, light west/southwest wind, trace of snow possible.

In the south-central portion of the region on Monday a storm slab avalanche released naturally on an east facing feature between 2200 and 2500 m, failing on the mid-December weak layer. Explosive control work in the central portion of the region produced a size 2.0 avalanche on a west facing slope at 2000 m. This avalanche initially failed on the early January interface before stepping down to the late November crust. A size 3.0 wet slab avalanche was reported from a steep south facing alpine feature in the mid afternoon when warm temperatures and direct solar input were most intense. On Sunday a natural persistent slab avalanche cycle was observed on south and southeast facing terrain between 2100 m and 2500 m, producing avalanches to size 2.5. These were running on both the early January and mid-December weak layers. Loose wet avalanches were reported on southwest, south and southeast facing terrain between 1700 m and 2800 m to size 2.5. On Saturday control work produced storm slab avalanches to size 2 on south and southeast facing alpine features. A cornice failure was also reported from a south/southeast facing alpine feature

Recent warm temperatures and strong solar input have left a crust that has been widely reported from many locations, high elevation north is likely one of the few crust-free zones. Fresh surface hoar up to 10 mm in size has been reported to ridgetop. We can probably expect a touchy storm slab to form on this interface as storm totals exceed 10 cm.There are three significant and active Persistent Weak Layers (PWL) that we are monitoring.The first PWL is known as the early January interface, it is 10 to 60 cm below the surface. It is composed of surface hoar on sheltered slopes as well as sun crust on steep solar aspects and is present at all elevation bands. Recent snowpack tests have shown moderate planar results at this interface.The second PWL is the mid-December facet/surface hoar/crust combination that is buried 40 to 100 cm deep and is most problematic at and below treeline. This interface has also shown sudden planar results in recent snowpack tests. The third and most deeply buried PWL is the late November rain crust. It is found 90 to 150 cm below the surface. This may be triggerable in thin spots around variable snowpack areas in the alpine.