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Avalanche Forecast

Archived

Apr 2nd, 2022–Apr 3rd, 2022

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

Regions

Kootenay Boundary.

Watch for isolated wind slabs near ridgecrest as we shift back into a pretty wintery weather pattern over the next few days.

Confidence

Moderate - Forecast snowfall amounts are uncertain.

Weather Forecast

SATURDAY NIGHT: No significant precipitation expected, light west/southwest wind, freezing level near valley bottom.

SUNDAY: Broken cloud cover at dawn building to overcast by lunch, no significant precipitation expected during the day, moderate southwest wind, freezing level around 1500 m. 5 to 10 cm expected Sunday night.

MONDAY: Overcast, 15 to 20 cm of snow possible, strong southwest wind, freezing level around 1500 m.

TUESDAY: Broken cloud cover, no significant precipitation expected, moderate west wind, freezing level around 1500 m.

Avalanche Summary

Aside from a bit of minor pinwheeling, no new avalanches reported since last Tuesday, when natural avalanche activity was observed on all aspects to size 3. A size 2 wet slab avalanche was rider triggered on a south facing treeline slope, failing on the crust buried in early March.

Snowpack Summary

Small pockets of wind slab may sit on north and east facing slopes at higher elevations. The upper snowpack is going through a daily melt-freeze cycle. A crust exists on all aspects to around 2500 m. Warm temperatures and sun may soften or break down the crust during the day and create moist snow. At very low elevations, the snowpack may be wet and isothermal, depending on overnight freezing levels. 

At 40 to 70 cm below the snow surface a sun crust exists on solar aspects, and weak surface hoar crystals sit on shaded aspects from early March. Reports suggest this layer is bonding well. The mid and lower snowpack are generally strong and well settled.

Terrain and Travel

  • Watch for wind-loaded pockets especially around ridgecrest and in extreme terrain.
  • Wind slabs may be poorly bonded to the underlying crust.
  • When a thick, melt-freeze surface crust is present, avalanche activity is unlikely.

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.