North Columbia

We've weathered the storm but we're not out of the woods yet. There's a great blog post on critical factors to watch out for this spring. Click here for details.

Moderate - Due to the number of field observations

We're looking at classic unsettled spring weather for the forecast period: cloudy with isolated (sometimes intense) flurries.TUESDAY: Isolated flurries (local amounts 5-10cm possible) / Light to moderate southeast wind / Freezing level 1500mWEDNESDAY: Broken skies with isolated flurries (local amounts 5-10cm possible) / moderate south wind /Freezing level 1600mTHURSDAY: Flurries in the morning with 5cm possible / Moderate southwest wind / Freezing level 1400m

We had a widespread natural avalanche cycle (to Size 4.5) at all elevations and aspects during the recent storm, including multiple adjacent avalanche paths running simultaneously with 1 Km wide propagation.Many of these avalanches ran in the storm snow with some also stepping down to persistent weaknesses (see snowpack summary below) deeper in the snowpack. Widespread wet slabs and loose wet avalanches were also reported below treeline.Of particular concern are the ongoing large destructive avalanches (some scrubbing to ground) that have been occurring daily: one or two deep spooky avalanches in each bulletin region of the Columbia Mountains. See the link in the headline for detailed discussion of these low probability, high consequence events.

We had heavy wet snow (or rain up to 2000m in places) and strong to extreme southerly winds during the weekend's storm. Temperatures also warmed up significantly. The end result: Widespread storm slabs and wind slabs at treeline and above, with significant cornice growth as well.The most recent storm snow (totals of 40-80cm) sits on older windslabs (or soft slabs) at treeline and above. Below 1800m, the new snow (with a thin breakable surface crust) sits on a melt-freeze crust from rain events last weekend. Reports so far are that the new snow is bonding well to the old crust, but that the storm snow instabilities are showing some reactivity to rider traffic.Approximately 100-140 cm below the surface you may find the late-February persistent weakness / crust interface. This layer has woken up from time to time as smaller avalanches still have to potential to 'step down' and trigger this layer.The deep mid-December facet layer (and November raincrust) still linger at the bottom of the snowpack and are the suspected culprit (running to ground) in a Glacier National Park avalanche. See here for the spooky picture.