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Avalanche Forecast

Archived

Nov 26th, 2014–Nov 27th, 2014

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

Regions

Purcells.

Winter storm conditions have produced a storm slab which sits on a touchy weak layer.  Now is a good time to avoid avalanche terrain and stick to low angle slopes.

Confidence

Poor - Due to the number of field observations

Weather Forecast

A warm, moist Pacific storm will continue to bring heavy precipitation to the southern interior on Thursday. The southern Purcells can expect to see a substantial rise in the freezing level on Thursday whereas the north of the region may stay cool. An Arctic high pressure is expected to arrive on Friday morning bringing cold, sunny conditions for the weekend. Weds. Night/Thursday: Precipitation 10-20mm, freezing level around 2000m, lower in the north, ridgetop wind strong SW Thurs. Night: Precipitation 5-10mm, ridgetop wind strong SWFriday: A mix of sun and cloud, light flurries possible, freezing level valley bottom, ridgetop wind easing during the daySaturday: A mix of sun and cloud, treeline temperature around -15C, ridgetop wind light N

Avalanche Summary

There are no new field reports from the Purcells. Recent reports from Rogers Pass include widespread natural activity up to size 3.  The storm snow in Purcells may not yet be enough for widespread natural activity but the warming on Thursday should produce some natural activity, especially in wind loaded areas.  Please help us improve this forecast and send observations to [email protected]

Snowpack Summary

This is an estimate of what the snowpack may look like based on a few old observations and previous weather. If you plan on heading into the mountains be sure to supplement this with your own observations and please pass along any data you collect ([email protected]).Around 30-50 cm of recent storm snow has fallen in the past few days. This new snow may be sitting on a layer of surface hoar, facets, and/or a sun crust (similar to the South Columbia). Below this you will likely find a 15-25cm thick layer of sugary facets, which is sitting on a solid rain crust from early November. Recent strong and variable winds have probably created dense wind slabs in exposed terrain and resulted in variable snow distribution in the alpine. At lower elevations, expect travel to be difficult and potentially hazardous as many early season hazards are exposed or lightly buried (stumps, logs, rocks, open creeks, etc).

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 Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.