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Avalanche Forecast

Archived

Mar 1st, 2023–Mar 2nd, 2023

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

Regions

South Coast, North Shore, Sasquatch, Sky Pilot, Tetrahedron.

6:30 AM PST UPDATE: Another 15 cm of new snow blanketed the region overnight. Natural avalanche activity is possible at all elevations on Thursday. Storm slab reactivity may persist for longer than typical, due to the weak surface they are sitting on. Human triggering remains likely.

Confidence

Moderate

Avalanche Summary

On Tuesday, a few natural storm slab avalanches were reported at treeline and below treeline elevations up to size 2. Most of the slabs were 30 cm deep with one significant one being 60 cm deep. Skier-controlled dry loose avalanches were easily triggered up to size 1 from steep terrain features on all aspects.

Last weekend, a widespread natural cycle occurred throughout the region. Reports came in of very touchy human-triggered storm slabs (size 1-2) averaging 30-60 cm deep and up to 100 cm deep in wind-loaded areas.

Storm slab reactivity is expected to persist for longer than is typical due to the weak surface they are sitting on.

Check out last Friday's North Shore Snowpack Update for a picture of the unusual snowpack setup leading into last weekend's storm.

Snowpack Summary

Another storm tonight could bring 20+ cm of new snow to all elevations above the 50-70 cm that has accumulated since last weekend. The recent cold temperatures have kept the snow mostly dry and unconsolidated, however, storm slabs will likely be more reactive with the additional load from wind, rising temperatures, and more snow. The recent snow will likely have a poor bond to the underlying old snow surfaces. This interface consists of weak faceted snow, old hard wind slabs, and a crust between 1100 and 1600 m.

The mid and lower snowpack is well-settled, strong, and consolidated.

Snowpack depths are reaching 250 cm at treeline.

Weather Summary

Wednesday Night

New snow 20 to 30 cm. Treeline temperatures -5°C. Ridge wind southwest 30 to 60 km/h. Freezing level 300 m.

Thursday

Cloudy with snow up to 10 cm. Possible sunny breaks and treeline temperatures -4 °C. Southwest wind 25 to 60 km/h. Freezing level 600 m.

Friday

Snow amounts 10-15 cm. Ridgetop wind 20 to 55 km/h from the southwest. Treeline temperatures -3 °C. Freezing level 500 m.

Saturday

Cloudy with isolated flurries. Treeline temperatures near 1 °C. Ridge wind southwest 15 km/h gusting to 40 km/h. Freezing level 1000 m.

More details can be found in the Mountain Weather Forecast.

Terrain and Travel Advice

  • Avoid all avalanche terrain during periods of heavy loading from new snow, wind, or rain.
  • Storm slab size and sensitivity to triggering will likely increase through the day.
  • Keep your guard up at lower elevations. Storms slabs have been reactive at all elevations.
  • Loose avalanches may start small but they can grow and push you into dangerous terrain.

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.

Loose Dry

Loose Dry avalanches are the release of dry unconsolidated snow and typically occur within layers of soft snow near the surface of the snowpack. These avalanches start at a point and entrain snow as they move downhill, forming a fan-shaped avalanche. Other names for loose-dry avalanches include point-release avalanches or sluffs.