Dashboard Regions Weather Stations Radar Alerts Glossary
Contact About
Log In

Register for an account and never miss a forecast again!

Register

Avalanche Forecast

Archived

Feb 25th, 2016–Feb 28th, 2016

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

Regions

Waterton Lakes.

Fast travel will reward those who get out early. Bring ski crampons for the morning and skin wax for the afternoon. JH

Weather Forecast

A trailing warm front spinning off of an Aleutian low pressure center will bring an end to the clear skies and cool weather we have been enjoying. Current models are predicting a warming spike for Friday afternoon, with freezing levels as high as 3300m. Saturday will be cloudy with scattered flurries and freezing levels up to 2200m.

Snowpack Summary

The upper snowpack is now well settled, with a surface crust forming overnight on solar aspects and breaking down with mid-day warming. At treeline and in the alpine a crust down 30-55cm persists as a concern. Widespread below 2200m and extending into the alpine on solar aspects, this was responsible for several large avalanches last week.

Avalanche Summary

A few loose wet avalanches up to size 1.0 were observed on solar aspects below treeline today. Otherwise there has been no new activity since last weekend.

Confidence

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.