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Avalanche Forecast

Archived

Apr 2nd, 2025–Apr 3rd, 2025

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

Regions

South Okanagan, Shuswap, North Okanagan.

Small slabs may be present in the alpine and are most likely to trigger in wind affected terrain.

Confidence

High

Avalanche Summary

No new avalanches were reported on Tuesday.

NOTE: Observations in this region are currently very limited.

Snowpack Summary

Up to 20 cm of recent snow overlies a 10 to 15 cm crust. Beneath this is a moist upper snowpack.

The mid/lower snowpack is well settled and strong.

Weather Summary

Wednesday Night

Mostly clear. 20 to 30 km/h northwest ridgetop wind. Treeline temperature -6 °C. Freezing level valley bottom.

Thursday

Sunny. 10 to 20 km/h north ridgetop wind. Treeline temperature -3 °C. Freezing level 1600 m.

Friday

Sunny. 5 to 10 km/h northwest ridgetop wind. Treeline temperature 0 °C. Freezing level 1900 m.

Saturday

Sunny. 10 to 20 km/h south ridgetop wind. Treeline temperature 5 °C. Freezing level 2700 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avalanche activity is unlikely when a thick melt-freeze crust is present on the snow surface.
  • Use caution above cliffs and terrain traps where even small avalanches may have severe consequences.

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.