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Avalanche Forecast

Archived

Apr 19th, 2023–Apr 20th, 2023

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

Northwest Coastal, Nass, Rupert, Shames, Stewart, Ningunsaw.

Fresh and reactive wind slabs may exist on leeward slopes in the alpine.

Numerous large persistent slab avalanches were triggered by riders in the alpine during the past week. This problem may continue to linger. Choose well-supported, low-consequence lines.

Confidence

Low

Avalanche Summary

On Wednesday, a glide slab size 2.5 was reported. Reports indicate it happened Tuesday afternoon. A few natural wet loose avalanches were seen up to size 2 from steep solar aspects.

Two persistent slab avalanches were reported northwest of Terrace last Wednesday (April 12th). A skier triggered size 2 on a north aspect in the alpine and a size 2.5 on an east aspect in the alpine that was triggered by solar radiation. Both failed on a layer of weak facets and/or surface hoar down 40-50 cm.

A fatal avalanche occurred north of Stewart last Tuesday (11th). It was a skier-triggered size 3 persistent slab avalanche that occurred on a northeast aspect in the alpine.

Observations are limited at this time of year, please consider sharing any information or photos you have on the Mountain Information Network to help guide our forecasts.

Snowpack Summary

10-20 cm of recent snow and strong southeast wind formed wind slabs that may remain reactive to human triggers in isolated locations in the alpine and possibly at treeline. A crust exists up to ridgetop on south-facing slopes and on all aspects up to 1300 m (ish).

The primary concern is two buried weak layers down 40-140 cm deep in most areas. They include facets and surface hoar in shaded areas and a melt-freeze crust elsewhere. Numerous human-triggered persistent slab avalanches have occurred on these layers during the past week.

The mid and lower snowpack is considered generally strong and well-bonded. In the far northern reaches of the region, basal facets may exist which are currently considered inactive. This layer may become active with abrupt changes to the snowpack, such as rapid loading (heavy snowfall or rain) or prolonged warming.

Weather Summary

Wednesday Night

Trace of new snow. Ridgetop winds 40-50 km/h from the southeast. Temperature at treeline around -5 C and freezing level valley bottom.

Thursday

Mostly cloudy. Ridgetop wind 30-50 km/h from the southeast. Temperature at treeline around -3 C freezing level 1300 m.

Friday

Mix of sun and cloud. Ridgetop wind 15-20 km/h from the southwest. Temperature at treeline around -3C with freezing level 1100 m.

Saturday

Cloudy with 5-15 mm of precipitation. Ridgteop wind 30-50 Km/h from the southwest. Temperature at treeline -3 C with freezing levels near 1100 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • If triggered, wind slabs avalanches may step down to deeper layers resulting in larger avalanches.
  • Potential for wide propagation exists, fresh slabs may rest on surface hoar, facets and/or crust.
  • Watch for signs of instability like whumpfing, hollow sounds, shooting cracks or recent avalanches.
  • Use conservative route selection. Choose simple, low-angle, well-supported terrain with no overhead hazard.

Problems

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.

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.