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Avalanche Forecast

Archived

Mar 15th, 2019–Mar 16th, 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 possible, human triggered probable.
Treeline
Natural avalanches possible, human triggered probable.
Below Treeline
Natural avalanches unlikely, human triggered possible.

Regions

South Rockies.

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

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

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind slabs that form over a persistent weak layer (surface hoar, depth hoar, or near-surface facets) may be termed Persistent Slabs or may develop into Persistent Slabs.

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.