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Avalanche Forecast

Archived

Mar 1st, 2023–Mar 2nd, 2023

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 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

North Rockies, Kakwa, McGregor, Pine Pass, Tumbler.

Make a plan to step back from avalanche terrain and away from overhead hazard as the storm progresses and avalanche danger increases over the day. Surface slides entraining recent accumulations or stepping down to the previous storm interface could result in surprisingly large and destructive avalanches.

Confidence

Moderate

Avalanche Summary

Observations since the weekend storm have shown mainly small dry loose avalanches releasing naturally, especially on steep, sunny slopes, as well as with skier traffic. We expect some degree of a slab avalanche cycle also took place at higher, wind affected elevations over the weekend, particularly in areas like Pine Pass and the MacGregors, where up to about 40 cm of new snow accumulated with strong southwest winds.

Earlier in last week there was evidence of deep persistent slab activity that occurred during a previous storm with avalanches up to size 3.5. While we currently expect the deep weak layer to be dormant, riders should continue to avoid steep, thin, rocky slopes where triggering a deep persistent avalanche would be most likely, particularly near alpine ridgelines.

Looking forward, moderate snowfall and high winds are expected to trigger an uptick in natural avalanche activity and human triggering potential through Thursday.

Snowpack Summary

Roughly 10-20 cm of new snow is expected to accumulate in the region by end of day Thursday. For the most part it will add to low density storm snow from the weekend (20-40 cm of it in the west of the region, closer to 5-15 in the east), but it may also bury recent wind slabs in more exposed areas.

The recent variable storm totals overlie faceted (sugary), heavily wind affected snow from previous cold temperatures and north winds. This interface remains somewhat in question with storm slabs being generally slow to form over it in recent days.

The middle of the snowpack is generally strong.

A weak layer of large and weak facets is found near the base of the snowpack. The layer is currently considered dormant, except perhaps in very steep alpine terrain that is inherently shallow. Riders should continue to avoid thin, rocky terrain where the likelihood of triggering this layer is higher.

Weather Summary

Wednesday night

Continuing snowfall bringing 5-10 cm of new snow. Strong to extreme southwest winds.

Thursday

Cloudy with continuing snowfall bringing 5-15 cm of new snow, continuing overnight. Strong southwest winds easing over the day. Treeline high temperatures around -9.

Friday

Cloudy with easing flurries bringing up to about 5 cm of new snow, including overnight amounts. Storm totals to 25-35 cm. Moderate southwest winds. Treeline high temperatures around -10.

Saturday

A mix of sun and cloud with isolated flurries. Light to moderate northeast winds. Treeline high temperatures around -15.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Use increased caution at all elevations. Storm snow is forming touchy slabs.
  • Watch for newly formed and reactive wind slabs as you transition into wind affected terrain.
  • Avoid shallow, rocky areas where the snowpack transitions from thick to thin.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.