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Avalanche Forecast

Archived

Apr 10th, 2014–Apr 11th, 2014

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.
Alpine
Natural avalanches unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Kootenay Boundary.

Confidence

Fair - Timing or intensity of solar radiation is uncertain

Weather Forecast

Friday: Dry with a mix of sun and cloud. Freezing level 2100 m. Ridgetop  winds 20-30 km/h from the west. Saturday: Starting out sunny, clouding over later on with a chance of showers. Freezing level around 1800 m. Calm winds. Sunday: Dry with a mix of sun and cloud. Freezing level 1900 m. Calm winds.

Avalanche Summary

No avalanches were reported on Wednesday. On Tuesday, high daytime temperatures triggered numerous loose wet avalanches up to size 1.5 on all aspects and at all elevations.

Snowpack Summary

Pronounced warming in the upper snowpack at all elevations has made the top 50 cm or more of the snowpack moist. Subsequent cooler temperatures have re-frozen the surface at higher elevations, although solar aspects at all elevations continue to undergo daily melt-freeze cycles. Several older melt-freeze crusts in the upper 40 cm are breaking down, although deeper crusts are reported to still be hard. The late January/early February persistent weak layer is deeply buried, but has not produced avalanches in this region for some time now.

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.