Regions
Banff Yoho Kootenay.
http://www.pc.gc.ca/apps/links/goto_e.asp?destination= Its time to step way back in terms of terrain choices and exposure, and let this spring cycle clean up the mountains. AM danger will be lower, but be out of all avalanche terrain by the time the day heats up as the change will happen quick.
Weather Forecast
A decent freeze tomorrow AM but again temperatures will spike rapidly with valley bottom highs in the 10-15C range, and 3000m temperatures approaching 0C. Skies will be very clear and winds mainly calm. This heat peaks on Wednesday but stays warm until next weekend.
Snowpack Summary
Sun crusts or moist snow on solar aspects and moist snow at lower elevations. 15-50 cm of snow has accumulated since March 7. This sits over a mix of facets, sun crust and wind slabs above treeline, and over 30-50 cm of weak facets elsewhere. While a supportive mid-pack exists in thicker areas, weak facets to the ground are seen in many thin areas.
Avalanche Summary
A widespread spring avalanche cycle has started, with the bulk occurring on solar aspects. Avalanche size ranged from size 1-3. Most slides have been within the surface snow (March 7 interface) with some stepping down a bit deeper; however, we have seen only a few avalanche step down to the basal layers.
Problems
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.
Persistent Slabs
Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.
Deep Persistent Slabs
Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.