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Avalanche Forecast

Archived

Apr 2nd, 2019–Apr 3rd, 2019

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

Regions

South Coast.

Forecast precipitation Tuesday night and Wednesday is expected to fall as snow at uppermost elevations in the South Coast mountains.

Confidence

Moderate - Intensity of incoming weather systems is uncertain

Weather Forecast

TUESDAY NIGHT: Rain or wet snow, accumulation 5-10 cm at upper elevations / light southeast wind / alpine temperature 0 C / freezing level 1600 mWEDNESDAY: Rain or wet snow, accumulation 5-10 cm at upper elevations / moderate southwest wind / alpine temperature -1 C / freezing level 1500 mTHURSDAY: Mainly cloudy / moderate south wind / alpine temperature 1 C / freezing level 1700 mFRIDAY: Periods of rain or wet snow / moderate south wind / alpine temperature 1 C / freezing level 1700 m

Avalanche Summary

No new avalanches have been reported recently.

Snowpack Summary

At uppermost elevations, 10-20 cm of new snow is likely sitting on a crust or wet snow. Below that, the upper snowpack is mostly moist or wet. At lower elevations precipitation is falling as rain onto an already moist or wet snowpack.

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.