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Avalanche Forecast

Archived

Mar 27th, 2019–Mar 28th, 2019

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

Regions

Jasper.

Good skiing can be found on sheltered and shady aspects up high. Don't forget your sunscreen, the sun has got some punch this time of year.

Weather Forecast

A warm dry airmass will remain over our area until the weekend. Thursday: A mix of sun and cloud. Precipitation: Nil. Treeline temperature: Low -12C, High -1C. Light ridge wind. Freezing level: 2200 metres.

Snowpack Summary

5-25cm of new snow (more in the Jasper area than near the Icefields), was redistributed by moderate N winds in the alpine, is settling fast and generally bonding well to previous surfaces. The entire snowpack is isothermal below treeline. On shady alpine aspects the snowpack remains dry.

Avalanche Summary

A few small solar triggered loose snow avalanches were observed in the backcountry adjacent to Marmot basin today.Share your observations with the community on the CAA Mountain Information Network

Confidence

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.

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.