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Avalanche Forecast

Archived

Apr 13th, 2019–Apr 14th, 2019

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

Regions

South Coast.

15-25 cm of snow on Saturday created fresh storm slabs at treeline and above. Pay attention to changing conditions with elevation on Sunday.

Confidence

High -

Weather Forecast

SATURDAY NIGHT: Cloudy with flurries; 3-5 cm. / Moderate, westerly winds / Alpine low -2 C / Freezing level 1000 m.SUNDAY: Mostly cloudy / Light, westerly winds / Alpine high -2 C / Freezing level 1000 m.MONDAY: Mix of sun and cloud / Light, southwesterly winds / Alpine high 1 C / Freezing level 1300 m.TUESDAY: Cloudy with flurries; 3-5 cm / Light, southwesterly winds / Alpine high 2 C / Freezing level 1500 m.

Avalanche Summary

No new avalanches have been reported in the region on Friday. However, avalanche activity is expected to increase on Sunday with the new snow and wind.

Snowpack Summary

15-20 mm. of precipitation on Saturday fell as moist snow at treeline and rain below which sits on a melt freeze crust. Warm temperatures and wet precipitation are producing a moist, spring snowpack. The snowpack depth decreases rapidly below 1200 m.

Problems

Storm Slabs

Storm Slab avalanches are the release of a cohesive layer (a slab) of new snow that breaks within new snow or on the old snow surface. Storm-slabs typically last between a few hours and few days (following snowfall). Storm-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.

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.