South Columbia

Cooler conditions should slowly improve stability but tricky conditions are still expected up high. Large slab avalanches still have the potential to release on deeply buried weak layers. Use extra caution on sunny slopes during the afternoon sun.

Fair - Due to the number of field observations

A ridge of high pressure brings a mix of sun and cloud for Thursday and Friday. Mainly dry conditions are expected with localized convective flurries possible. Freezing levels are forecast to reach around 1600m in the afternoon and drop to around valley bottom overnight. Alpine winds are expected to be light from the NW on Thursday and light from the SW on Friday. On Friday overnight and Saturday, a weak storm system should reach the interior. Light precipitation is expected with freezing levels reaching around 1500m and moderate alpine winds from the SW.

On Tuesday, two natural size 1.5-2 wind slabs were reported above 2400m elevation. Some natural cornice failures also triggered storm slabs up to size 2. Most of this activity is expected to have occurred in the recent storm snow. On Monday, several natural slab avalanches were reported above around 2200m elevation as well as lots of wet sluffing at lower elevations. Some of these were up to 1m deep and these are expected to be failing on persistent weak layers. Ongoing persistent slab, storm slab, and loose wet avalanches have been occurring since last Friday. Activity is now expected to taper off with the cooler temperatures. Natural avalanches are generally not expected on Thursday except possibly on steep sun-exposed slopes in the afternoon. Human-triggered wind slabs and persistent slabs are still a concern, especially on steep, unsupported slopes in the alpine. Stability is generally expected to improve with the cooling trend but this may take a few days at higher elevations and tricky conditions may still exist on Thursday.

The upper snowpack likely contains multiple new crust layers. The most prominent of these new crusts is likely a thick rain crust down 20-40cm that formed last Friday when it rained into the alpine. Another crust likely exists near the surface but may be buried under 5-15cm of dry snow that fell on Tuesday after the temperatures dropped. These near surface crust layers likely extend well into the alpine. In the high alpine, strong winds have redistributed the new snow and wind slabs can be expected in leeward terrain features. Several persistent weak layers exist in the upper 1m of the snowpack and remain a concern. The mid-March crust/facet layer is down around 60cm and has been reactive to light triggers recently. Down around 80cm is the mid-February crust/facet/surface hoar layer which has also been reactive to heavy loads like avalanches in motion stepping down, cornice failures, or explosives. Both layers have the potential for wide propagations and very large avalanches are still possible.