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Avalanche Forecast

Archived

Mar 29th, 2025–Mar 30th, 2025

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

Regions

Sasquatch, Sasquatch, Coquihalla, Harrison-Fraser, Manning, Skagit.

Sunshine can have a powerful effect on stability and your desire to push into aggressive terrain. Where buried weak layers may exist, build margins into your terrain choices.

Confidence

Low

Avalanche Summary

Reports have been very limited in this region. No avalanches have been reported since Tuesday, when a size 3.5 persistent slab was observed on a north alpine face that likely failed last weekend. Several loose wet avalanches on sunny slopes were also observed in this MIN post.

Please consider sharing your observations to the MIN.

Snowpack Summary

Up to 15 cm of snow from Saturday sits over wet or crusty surfaces. On all but high north-facing alpine slopes, the upper snowpack is wet. Below 1800 m, it has melted substantially.

A persistent weak layer of facets and surface hoar from February is now 90 to 150 cm deep, and a layer of facets and surface hoar from late January is buried 110 to 190 cm. These layers remain a concern, especially in the south and eastern parts of the region where the overall snowpack is shallower. Otherwise, the snowpack is generally well-settled and strong.

Weather Summary

Saturday night

Clearing. 5 to 15 km/h variable ridgetop winds. Treeline temperature -2 °C. Freezing level dropping to 1000 m.

Sunday

Sunny. 20 to 40 km/h southeast ridgetop winds. Treeline temperature +2 °C. Freezing level rising to 2000 m.

Monday

Cloudy, with 5 to 15 cm of snow above 1400 m, rain below. 15 to 30 km/h southwest ridgetop winds. Treeline temperature -2 °C. Freezing level 1500 m.

Tuesday

Cloudy, with 5 to 10 cm of snow. 20 to 30 km/h southwest ridgetop winds. Treeline temperature -2 °C. Freezing level 1500 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • A moist or wet snow surface, pinwheeling, and natural avalanches are all indicators of a weakening snowpack.
  • The more the snowpack warms up and weakens, the more conservative your terrain selection should be.
  • In areas where deep persistent slabs may exist, avoid shallow or variable depth snowpacks and slopes above cliffs.
  • Cornice failures could trigger large and destructive avalanches.

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.

Loose Wet

Loose Wet avalanches are the release of wet unconsolidated snow or slush. These avalanches typically occur within layers of wet snow near the surface of the snowpack, but they may quickly gouge into lower snowpack layers. Like Loose Dry Avalanches, they start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-wet avalanches include point-release avalanches or sluffs. Loose Wet avalanches can trigger slab avalanches that break into deeper snow layers.

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.