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Avalanche Forecast

Archived

Mar 28th, 2019–Mar 29th, 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.
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, human triggered possible.

Regions

Jasper.

You can expect a localized rise in avalanche hazard depending on exposure to the sun. Latest report from the field is, high probability for a serious goggle tan. Moral of the story: Start early. wear sunscreen and call your Mother, she misses you!

Weather Forecast

Mixed sun and cloud for Friday. Freezing level got to approx. 2400m on Thursday. Overnight temperatures have been near -10 and will swing up to as high as +5 on Friday, though it will feel much warmer in the sun.

Snowpack Summary

New snow is settling fast and generally bonding well to previous surfaces. The snowpack is cycling from isothermal, to overnight freeze with an inconsistent, supportive crust below (about 10cm thick) at treeline on all aspects. Crust breaking down by mid-morning on all solar aspects.

Avalanche Summary

A few small solar triggered loose snow avalanches were observed in the back-country adjacent to Marmot basinShare 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.