Avalanche Forecast

Issued: Mar 15th, 2019 5:35PM

The alpine rating is moderate, the treeline rating is moderate, and the below treeline rating is moderate. Known problems include Wind Slabs and Persistent Slabs.

Avalanche Canada jleblanc, Avalanche Canada

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We're expecting mostly cloudy conditions on Saturday, but slopes receiving direct sun could produce loose wet avalanches surprisingly quick.

Summary

Confidence

Moderate - Timing or intensity of solar radiation is uncertain

Weather Forecast

FRIDAY NIGHT: Partly cloudy, alpine low temperature of -5C, moderate westerly winds at ridgetop.SATURDAY: Cloudy with sunny periods, alpine high temperature of -2C, light west wind, freezing level between 1600m and 1800m. SUNDAY: Sunny with cloudy periods, alpine high temperature near 0C, light west wind, freezing level around 2000m, no overnight re-freeze expected.MONDAY: Mainly sunny, alpine high temperature of +3C, light west wind at ridgetop, freezing level around 2500m, no overnight re-freeze expected

Avalanche Summary

Two notable large natural persistent slabs releases were observed on northwest slopes at treeline on Thursday. A few natural avalanches (up to size 1.5), mainly dry-loose and thin wind slabs were also observed on steep slopes. Ridders were surprised to remotely trigger a small persistent slab avalanche down 60 cm late Thursday afternoon on a west facing slope below treeline. See the MIN report from Lizard Range and Flathead for more details. With the upcoming warming natural avalanches are increasingly likely as the sun impacts solar aspects.

Snowpack Summary

Moderate to strong southwest winds have affected the low density storm snow at and above treeline, building winds slabs near ridgetop and behind lee features. These fresh slabs overly old slab slabs in alpine terrain. The sun has transformed the recent 15-20 cm of storm snow which became moist on southerly aspects at lower elevations. The middle snowpack consists of weaker faceted snow with few if any distinct layers. In isolated wind protected locations a thin surface hoar layer from mid-January is 50-80 cm deep. The surface hoar is most prominent in the Elk Valley between 1600 m and 1900 m. Regardless of whether they are facets or surface hoar crystals, when the weather warms they may produce avalanches on steep unsupported slopes.

Problems

Wind Slabs

An icon showing Wind Slabs
Wind blowing from various direction has formed slabs in unexpected areas. Newly formed slabs may be more reactive than expected with this intense warming and direct sunlight.
If triggered wind slabs may step down to deeper layers resulting in large avalanches.Sun exposed slopes can quickly become unstable as the surface gets moist or wet.Be careful in shallow snowpack areas where triggering is more likely.

Aspects: All aspects.

Elevations: Alpine, Treeline.

Likelihood

Possible - Likely

Expected Size

1 - 2

Persistent Slabs

An icon showing Persistent Slabs
Although the likelihood of triggering a persistent slab is fairly low, the consequences can be severe as the weak layer is deep in the snowpack.

Aspects: All aspects.

Elevations: Treeline.

Likelihood

Unlikely - Possible

Expected Size

1 - 2.5

Valid until: Mar 16th, 2019 2:00PM

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