Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Alpine
Natural avalanches unlikely, human triggered possible.
Treeline
Natural avalanches unlikely, human triggered possible.
Below Treeline
Natural avalanches unlikely.
Regions
South Rockies.
This bulletin was published using very limited field data. You can help by using the new Mountain Information Network. For more info, check out this blog post: http://www.avalanche.ca/blogs/VIYBuScAAJdbdqPz/m-i-n-intro
Confidence
Poor - Due to the number of field observations
Weather Forecast
A series of sub-tropical systems will make their way through the region on Wednesday and Thursday bringing light precipitation, freezing levels to about 2400m and strong southwest winds. By Friday, precipitation should taper-off dramatically with light southwest winds and freezing levels hovering at about 1500m.
Avalanche Summary
No avalanche activity reported. If you've witnessed any avalanches, please send a note to [email protected]
Snowpack Summary
Recent warming suggests snow surfaces are likely moist or wet at most elevations. There is at least one, maybe more, problematic layers in the South Rockies snowpack. Up to about 90cm of settled snow overlies a weak layer of facets and crusts which formed during November's dry spell. Not much is known about the reactivity of this layer, nor the slab above it. But, it doesn't take much of a leap of faith to understand that a meter deep slab sitting on a persistent weak layer is a potentially bad thing.
Problems
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.
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.