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Avalanche Forecast

Archived

Jan 25th, 2018–Jan 26th, 2018

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

Regions

Glacier.

Watch for storm slabs at treeline and alpine elevations. Keep the persistent weak layers in mind with your trip planning decisions.

Weather Forecast

The snow just keeps on falling with another 6cm forecast today accompanied by gusty SW winds and a 1400m freezing level.  Friday/Saturday looks like a lull between systems with cooler temperatures and moderate to light SW-S winds forecast. The next pulse of Pacific moisture is set to hit on Sunday.

Snowpack Summary

50cm+ storm snow in the last 3 days at 1900m and over 150cm of snow in the last 2 weeks. Winds light the last 24hrs but are up to mod S'ly this morning. Expect to find fresh windslab along ridge lines and lee features. The Jan 16 surface hoar is down ~50cm, Jan 4 down ~70 and Dec 15 down ~1m+ making for a complex sandwich of weak layers.

Avalanche Summary

No new natural avalanche activity observed yesterday with poor visibility. Avalanche control produced one size 1 and one size 2.5 on the Cutbank slide paths in the Beaver Valley.

Confidence

Due to the number of field observations

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.