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Avalanche Forecast

Archived

Feb 26th, 2020–Feb 27th, 2020

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.

Regions

Lizard-Flathead.

Cornice failure, loose wet avalanches and even slab avalanches are possible as the upper snowpack feels the strong sun and warming temps for the first time today. Really watch your exposure to overhead hazard, it would be easy to be surprised by weird avalanches today.

Confidence

Low - Uncertainty is due to the timing or intensity of solar radiation and its effect on the snowpack.

Weather Forecast

Clear skies and warm sun for the next couple of days...

WEDNESDAY NIGHT: Freezing level at valley bottom, light southwest wind at lower elevations, moderate to strong west/northwest wind at ridge top, no precipitation expected.

THURSDAY: A few clouds, freezing level starting at valley bottom rising to about 1700 m, light to moderate southwest wind at lower elevations, strong west wind at ridge top, no precipitation expected.

FRIDAY: Clear skies, freezing level starting near valley bottom rising to about 2200 m, light to moderate west/southwest wind, no precipitation expected. Freezing level holding around 1800 m Friday night.

SATURDAY: Broken cloud cover, freezing level lowering from 1800 m to 1500 m, light to moderate southwest wind, 3 to 6 cm of snow expected.

Avalanche Summary

Natural and human triggered wind and storm slabs to size 1.5 were observed Tuesday on north/northeast facing features above 1900 m. The human triggered wind slab avalanche is thought to have ran on the early February crust/facet combo. This MIN observation from Harvey Pass shows a skier triggered avalanche that looks like it could have run on surface hoar.

Widespread natural and intentionally human triggered avalanche activity to size 2 was reported from all aspects Monday. One of the wind slabs was up to 45 cm deep in places. The bulk of the activity was above 1750 m which suggests that wind loaded features near ridge line appear to be the problematic features.

Snowpack Summary

Sunday's storm produced 15 to 25 cm of storm snow that has settled to about 20 cm. This snow rests on a variety of old surfaces including a firm crust on solar aspects, soft faceted snow, possibly a spotty surface hoar layer and old wind slabs near ridge crest. The new snow has been formed into variable wind slabs in exposed terrain features, especially those near ridge crest.

A thick rain crust that has facets associated with it sits 30-60 cm below the surface and can be found up to ridge top. The avalanche listed above is the first activity that we've seen on the crust since February 17.  

The mid-pack is well settled and strong, but the base of the snowpack contains basal facets that are most prominent in shallow rocky start zones.

Terrain and Travel

  • Avoid freshly wind loaded features, especially near ridge crests, roll-overs and in steep terrain.
  • Use extra caution around cornices: they are large, fragile, and can trigger slabs on slopes below.
  • Loose avalanches may start small but they can grow and push you into dangerous terrain.
  • Keep in mind the crust offers an excellent bed surface for avalanches.
  • Avoid sun exposed slopes when the solar radiation is strong, especially if snow is moist or wet

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.