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Avalanche Forecast

Archived

Mar 8th, 2025–Mar 9th, 2025

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

Regions

South Okanagan, Shuswap, North Okanagan.

Triggering the buried weak layer is unlikely, but if triggered it will be a large avalanche.

Travel one at a time and watch your partner.

Confidence

Moderate

Avalanche Summary

Two large (size 2) storm slabs were triggered with explosives near Kamloops on Thursday.

Snowpack Summary

5 to 10 cm of snow covers a widespread melt-freeze crust, which in sheltered spots may have small surface hoar crystals on it, found treeline and below. The crust exists on all aspects, except possibly high-elevation north-facing slopes. 30 to 60 cm further down is a crust or surface hoar/facets.

A weak layer, buried in late January, consists of surface hoar, facets, and/or a crust, is found 50 to 90 cm deep.

Below this, the mid and lower snowpack is generally settled and strong.

Weather Summary

Saturday Night

Cloudy. 30 to 50 km/h south ridgetop wind. Treeline temperature 0 °C. Freezing level 1500 m.

Sunday

Cloudy with 0 to 5 cm of snow above 1500 m. 30 to 50 km/h southwest ridgetop wind. Treeline temperature -2 °C. Freezing level 1600 m.

Monday

A mix of sun and cloud with 5 to 10 cm of snow overnight. 20 km/h southwest ridgetop wind. Treeline temperature -5 °C. Freezing level 1200 m.

Tuesday

A mix of sun and cloud with up to 5 cm of snow overnight. 20 to 30 km/h southwest ridgetop wind. Treeline temperature -5 °C. Freezing level 1200 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Be mindful that deep instabilities are still present in the snowpack.
  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.
  • Avoid freshly wind-loaded terrain 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.