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Avalanche Forecast

Archived

Nov 27th, 2014–Nov 28th, 2014

Alpine
Natural avalanches possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.
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

Kootenay Boundary.

A Special Public Avalanche Warning is in effect. There seems to be a lot of variability in the snowpack across this region. Conditions are expected to be worse in the north.

Confidence

Poor - Due to the number of field observations

Weather Forecast

The current warm stormy flow is expected to be replaced by brutally cold arctic air this weekend.Friday: 10-25 mm precipitation. Temperatures are generally remaining warm, with a freezing level near 1900 m. Rapid cooling late in the day, which may lead to snow to low levels, and deep dry new snow at upper elevations. Strong to gale SW winds, easing as the cold air/snow arrives.Saturday: Any remaining snowfall should end by afternoon. Becoming cold and clear. Light winds.Sunday: Cold and clear. Light winds. Brrr.

Avalanche Summary

A widespread loose wet and wet slab avalanche cycle to size 2 was observed on Thursday at treeline and below in the south of the region. No observations were made in the alpine.

Snowpack Summary

Around Kootenay Pass, rain moistened (and weakened) the snowpack to perhaps about 2000m on Thursday. It's expected that the snowpack in this region may remain weak through the warm part of Friday, but strengthen rather quickly after the cold snap arrives.In the Whitewater backcountry, a weak and shallow snowpack was reported on Wednesday, with lots of whumpfing and collapsing. Due to a lack of field observations, it is unclear how Thursday's warm temperatures/ rain have influenced the snowpack here. Above about 2000m and in the north of the region, I have the most avalanche concerns. It's these areas which may be harbouring a weak layer (formed during November's dry spell), now overloaded with storm snow. We have very limited field information. If you have been out in the mountains, we'd love to hear from you. Please email us at [email protected].

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.