It is a good time to be traveling in the mountains, but be careful with fresh shallow wind slabs on all aspects near ridge crest, be mindful of the threat posed by large cornices and watch for small loose avalanches in the afternoon.
Weather Forecast
A gulf Alaska "mother low" continues to sling smaller lows at the province keeping temperatures cool and offering small amounts of precipitation to the Columbias. There is potential for a stronger system to move into the region this weekend, stay tuned for more details. THURSDAY: Broken cloud cover, freezing level beginning around 1000 m rising to about 1600 m, light northerly wind, 2 to 8 mm of precipitation possible.FRIDAY: Clear skies in the morning building to broken cloud cover in the afternoon, freezing level beginning around 500 m rising to about 1600 m, light to moderate southwest wind, trace of precipitation possible.SATURDAY: Broken cloud cover, freezing level holding around 1500 m, moderate to strong southwest wind, 2 to 4 mm of precipitation possible.
Avalanche Summary
No new avalanche activity reported from the region Tuesday. In the neighboring Glacier National Park, all aspects were involved as natural loose wet avalanches ran size 2.5 to 3 between 1950 and 2700 m.Loose wet avalanches to size 2 were reported from all aspects between 1000 and 2300 m Monday. In the neighboring Glacier National Park, loose wet avalanches to size 3 were reported from solar (south and west) aspects to size 3 between 2000 and 2300 m. A size 1.5 storm slab was ski cut from a northwest facing feature at 2400 m illustrating that isolated storm/wind slabs are still in play at upper elevations.On Sunday natural loose wet avalanches to size 2 were reported from all aspects (including north) as high as 2800 m.
Snowpack Summary
A thin surface crust is now present on all aspects to at least 2300 m. This crust likely goes even higher on south facing aspects, and there may be a bit of preserved cold snow on high elevation north facing features. There are now a few different crusts in the upper 50 cm of the snowpack, but they have not been problematic. Fresh wind slabs have started to form immediately lee of ridge crest, continued new snow and wind should fuel their development through the weekend.There is some lingering concern around the mid-March Persistent Weak Layer (PWL) in the alpine where it is found 60 to 110 cm below the surface. This buried crust/surface hoar interface was widely reactive last week, but has not produced any avalanche activity in the last few days. It is likely trending towards dormancy, but we need to keep it in the back of our minds as it is capable of producing large avalanches should it fail. Deeper persistent weak layers from December and January are dormant at this time.
Problems
Wind Slabs
Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.
Loose Wet
Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.