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Avalanche Forecast

Archived

Mar 17th, 2022–Mar 18th, 2022

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

Regions

Purcells.

Cautious route-finding is recommended right now due to uncertainty about buried weak layers, especially in the western parts of the region where there is potential for large avalanches.

 

Confidence

Moderate - Uncertainty is due to the complexity of the snowpack’s structure.

Weather Forecast

THURSDAY NIGHT: Cloudy with scattered flurries bringing up to 5 cm of new snow, light to moderate wind from the southwest, treeline temperatures drop to -8 with freezing level around 1200 m.

FRIDAY: Mostly cloudy with some light flurries bringing trace amounts of snow, light wind from the southwest, treeline temperatures around -4 C with freezing level around 1500 m.

SATURDAY: Mostly cloudy with flurries starting midday brining trace amounts of snow, moderate wind from the southwest, treeline temperatures around -4 C with freezing level around 1500 m.

SUNDAY: Flurries continue overnight with 5 to 10 cm of new snow by the morning then sunny breaks in the afternoon, light wind from the west, treeline temperatures around -6 C with freezing level around 1200 m.

Avalanche Summary

There were several notable human-triggered slab avalanches on Wednesday that suggested recent snow is bonding poorly to the underlying layers. These occurred on a range of aspects above 2000 m. Most slabs were small in the top 20 to 30 cm of snow (size 1), but one larger 70 cm thick slab was remotely triggered from below by a group of skiers (size 2). This avalanche occurred on a south aspect at 2250 m.

Over the past few days there have also been reports of cornice failures, small loose avalanches, and several large (size 2) wind slab avalanches in alpine terrain following Tuesday's storm.

While we are becoming less concerned about wind slabs, we have heightened concern about a developing persistent slab problem in some parts of the Purcells (read more in this blog).

Snowpack Summary

The upper snowpack is highly variable as snowfall totals over the past week have ranged from 20 cm in the eastern Purcells to 60 cm in the western Purcells. Snow depths also taper significantly with elevation, with moist and crusty surfaces below 1800 m and on south aspects into the alpine.

In some areas this snow is well bonded to old crust layers, while in other areas the snow has settled into a reactive slab above weak layers around the crusts. At this point, it appears persistent slab problems could be developing in the deeper snowpack areas along the western side of the range, while the eastern side more likely has thinner wind slabs. The lower snowpack is generally well bonded.

Terrain and Travel

  • Uncertainty is best managed through conservative terrain choices at this time.
  • Choose slopes that are well supported and have limited consequence.
  • Back off if you encounter whumpfing, hollow sounds, or shooting cracks.
  • Be carefull around freshly wind loaded features.

Problems

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.

Wind Slabs

Wind Slab avalanches are the release of a cohesive layer of snow (a slab) formed by the wind. Wind typically transports snow from the upwind sides of terrain features and deposits snow on the downwind side. Wind slabs are often smooth and rounded and sometimes sound hollow, and can range from soft to hard. Wind 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.