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Avalanche Forecast

Archived

Jan 27th, 2018–Jan 28th, 2018

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

Regions

South Coast.

Natural avalanche cycle expected on Sunday. Travel in avalanche terrain not recommended.

Confidence

High -

Weather Forecast

SUNDAY: 40-60 mm of rain (snow above roughly 1500m) / Strong to extreme southwesterly ridgetop winds / Freezing level rapidly rising to around 1800m.MONDAY: 60-80 mm of rain (snow above roughly 1500m) / Strong to extreme southwesterly ridgetop winds / Freezing level around 1800m.TUESDAY: 10-15 cm of new snow / Moderate southwesterly ridgetop winds / Freezing level dropping to around 800m.

Avalanche Summary

No new avalanches have been reported in this region on Friday. However, a natural avalanche cycle is expected to begin Saturday with the incoming storm.

Snowpack Summary

15-25cm of new snow is being redistributed by strong southwesterly ridgetop winds creating fresh storm slabs reactive to human triggers. Below the most recent storm snow there is a crust at treeline and below. The reactivity of the new storm slabs is likely to vary greatly depending on elevation/ temperature and orientation to wind. In general, I would expect the touchiest conditions to exist in exposed, higher elevation terrain.

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.

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.