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Avalanche Forecast

Archived

Jan 3rd, 2018–Jan 5th, 2018

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

Regions

Vancouver Island.

Travel/Terrain Advice

Avoid steep wind and storm loaded features especially as afternoon temps and freezing levels climb and certainly once the forecast rain begins to fall. This dangerous combination will potentially awaken the previous stubborn slabs. Small loose wet avalanches have the potential for high consequences near terrain traps. Avoid travel above cliffs, rocks and depressions. Steer clear of gullies where small snow amounts are magnified. Careful snowpack evaluation, cautious route finding and conservative decision making are key Thursday into Friday. Who wants to ski in the rain anyways?

Past Weather

No new snow in the forecast area with calm to light (5-17 km/h) variable direction winds. Daytime temps were mainly warm from 0-7 degrees in the alpine and treeline with cold temps only lingering in well shaded valley bottoms.

Avalanche Summary

Significant pinwheeling was observed on all aspects and elevations as freezing levels climbed over the past couple days. Trees were shedding their snow with the warm temps well up into the treeline. Intentional ski cuts produced small (size 1) loose wet avalanches at treeline at 1580 m on a NW aspect mid afternoon on January 1st on a steep unsupported slope in Strathcona Park.

Snowpack Summary

Surface - Rising freezing levels and warm temps during the day have caused moist surface conditions on all aspect and elevations. Possible cooling at night will produce a thin melt freeze crust. Upper - Moist heavy snow overlies previous lower density (light and fluffy) storm snow in wind sheltered zones, and in open exposed areas at treeline and alpine moderate-firm wind pressed slabs cap the lower density snow giving it a scary hollow feel. Mid - Well settled. Lower - Well settled.

Weather Forecast

Warm air up high and cold air in the valley bottoms will begin to fade Wednesday into Thursday as south west flows bring mild pacific air up coast. With this new system significant precipitation is expected Thursday-Friday most likely in the form of rain to the top of our summits. Wed - 0 mm. Winds light to moderate 3-15 km/h from the south east. Freezing levels of 700-2700 m Thurs - 5-15 mm most likely in the form of rain. Winds light to moderate 5-35 km/h from the southeast. Freezing levels of 700-2700 m Fri - 11-40 mm mainly in the form of rain, tapering to snow midday in the north and in the evening to the west and south. Winds strong south east tapering to light south 45-10 km/h. Freezing levels of 1000-2300 m

Confidence

High- good alpine, treeline and below treeline observations, weather forecast models in agreement.

Problems

Wet Slabs

Wet Slab avalanches are the release of a cohesive layer of snow (a slab) that is generally moist or wet when the flow of liquid water weakens the bond between the slab and the surface below (snow or ground). They often occur during prolonged warming events and/or rain-on-snow events. Wet Slabs can be very unpredictable and destructive.

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.