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Avalanche Forecast

Archived

Jan 27th, 2015–Jan 28th, 2015

Alpine
Natural avalanches unlikely.
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 unlikely.
Treeline
Natural avalanches unlikely.
Below Treeline
Natural avalanches unlikely.

Regions

Sea To Sky.

Observations from the high alpine (above 2300m) have been very limited. Dig down and test for weak layers before committing to steeper, exposed lines.

Confidence

Fair - Due to the number of field observations

Weather Forecast

Expect a mix of of sun and cloud for the forecast period. Winds are forecast to remain light to moderate from the northwest, switching to southwest on Thursday and Friday. Freezing levels should hover at 1200m on Wednesday, rise to 1800m on Thursday, and fall back to 1200m on Friday.

Avalanche Summary

No recent avalanches have been reported.

Snowpack Summary

Up to 50 cm of settled storm snow has been saturated by rain up to about 2100m. With the forecast cooling trend, most surfaces will likely be sporting a hard melt-freeze crust. At the highest elevations you might find dense, stubborn wind slabs in lee terrain. New cornice development has also been noted. The older storm snow overlies a hard crust and/or surface hoar layer which formed in early January. The bond at this interface will be largely elevation dependant as rain may have penetrated the snowpack enough to dissolve the crust in many areas. At higher elevations where snow has fallen, this interface may still be reactive although no recent avalanches have been reported at this interface.Deeper snowpack weaknesses seem to have become unreactive, and should become even less of a concern if the forecast cooling trend verifies.

Problems

Cornices

Cornice Fall is the release of an overhanging mass of snow that forms as the wind moves snow over a sharp terrain feature, such as a ridge, and deposits snow on the downwind (leeward) side. Cornices range in size from small wind drifts of soft snow to large overhangs of hard snow that are 30 feet (10 meters) or taller. They can break off the terrain suddenly and pull back onto the ridge top and catch people by surprise even on the flat ground above the slope. Even small cornices can have enough mass to be destructive and deadly. Cornice Fall can entrain loose surface snow or trigger slab avalanches.