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Avalanche Forecast

Archived

Nov 26th, 2018–Nov 27th, 2018

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

Regions

Purcells.

More snow and increasing winds increase the likelihood for slab avalanches to develop. If snowfall amounts exceed 25 cm, avalanche hazard will be higher than indicated.

Confidence

Low - Forecast snowfall amounts are uncertain

Weather Forecast

Snow forecasts identify the largest snowfall amounts occurring in the St Mary's drainage area of the Purcells forecast region.MONDAY NIGHT: Cloudy with flurries / Accumulation: up to 10 cm / Alpine temperature: Low -1C / Light southwest ridge wind / Freezing level 1500mTUESDAY: Cloudy with flurries / Accumulation: up to 15 cm / Alpine temperature: High +1C / Light to moderate southwest ridge wind / Freezing level 1500mWEDNESDAY: Cloudy with sunny breaks and flurries / Accumulation: up to 5 cm / Alpine temperature: high 0C / Moderate decreasing to light southwest ridge wind / Freezing level 1600mTHURSDAY: Cloudy with sunny periods / Accumulation: trace / Alpine temperature: High -1C / Light ridge winds

Avalanche Summary

On Saturday, a large human triggered avalanche was reported in the South Columbia forecast region. The size 3 avalanche occurred on a steep, north aspect in the alpine and failed to ground, likely on the October crust. This avalanche is notable for the Purcells where we have a similar, but shallower snowpack than in the South Columbia, resulting in a higher possibility of impacting a weak layer near the ground. Find the MIN report here.Small windslabs have been triggered by skiers and explosives in cross-loaded and lee terrain features at treeline and alpine elevations. Earlier in the month, a natural avalanche cycle took place over the late October crust/facet combination. Be aware of the continued possibility for smaller avalanches to 'step down' or even initiate at this deeper layer.

Snowpack Summary

Snowfall through Monday afternoon has deposited up to 10 cm around the region. This added to recent snow, has buried a surface hoar/sun crust layer down about 10-30 cm. Reports in the region show this variable layer sitting above a layer of recently reactive wind slab. This wind slab layer overlies yet another widespread layer of surface hoar from mid-November, now found about 30-50 cm deep. A final, prominent feature of the snowpack is a combination of a melt-freeze crust and underlying sugary, faceted snow found around the base of the snowpack. Avalanches have been triggered where there is a slab above this crust.

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.

Persistent Slabs

Persistent Slab avalanches are the release of a cohesive layer of snow (a slab) in the middle to upper snowpack, when the bond to an underlying persistent weak layer breaks. Persistent layers include: surface hoar, depth hoar, near-surface facets, or faceted snow. Persistent weak layers can continue to produce avalanches for days, weeks or even months, making them especially dangerous and tricky. As additional snow and wind events build a thicker slab on top of the persistent weak layer, this avalanche problem may develop into a Deep Persistent Slab.