Avalanche Forecast

Fair - Freezing levels are uncertain on Tuesday

Synopsis: A ridge of high pressure along the coast will move eastward across the interior Monday. The trailing pacific frontal system should bring increased cloudiness on Tuesday with the potential for light to moderate precipitation Wednesday above 1000m.Monday: Freezing Level: 1000m -1200m; Precipitation: Nil; Treeline Wind: Light, E | Ridgetop Wind: Moderate, WTuesday: Freezing Level: 1700m - 2300m; Precipitation: Trace; Treeline Wind: Light, SW | Ridgetop Wind: Strong, W Wednesday: Freezing Level: 800m - 1300m; Precipitation: 5:10mm - 5:15cm; Treeline Wind: Light, NE | Ridgetop Wind: Moderate, SW

Saturday's observations were limited to small loose snow avalanches on steep unsupported features.On Friday a few loose natural avalanches to size 2 were observed in steep alpine terrain. Explosive control work in the region produced size 2 avalanches that were only 10 - 30 cm in depth.On Wednesday a size 2 wind slab was accidentally triggered by a skier in the southeast corner of the region. The avalanche occurred on a northeast aspect at about 2600m.

See this great video from our South Rockies field team that does an awesome job of summarizing the current state of the snowpack.The region picked up 5 - 10cm of convective snowfall Saturday night which adds to the 60 - 100cm of storm snow fell in the last week. Winds have been out of the SW through NW which has created fresh wind slabs in lee terrain. Around 70 cm of settling storm snow rests on a graupel layer that can be found in much of the region. This makes for around 90 cm on top of the mid march crust at this point. This crust exists on all aspects below 2000m and on solar aspects in the high alpine. North of Sparwood and in the Crowsnest Pass area, the buried crust seems more specific to previously sun-exposed slopes. The deep facet/crust persistent weakness buried at the beginning of February (now down up to 150cm) seems unlikely to trigger in areas where the hard, supportive exists. No matter where you are in the region, this weakness should stay on your radar as any activity at this interface would be large and destructive. Possible triggers include a large cornice fall, a large input in a thin snowpack area or solar warming.Cornices have also become large and unstable.