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Avalanche Forecast

Archived

May 3rd, 2023–May 4th, 2023

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

Regions

Glacier.

A weak snowpack and strong May sun are making for high avalanche hazard. Backcountry travel is not recommended.

Confidence

High

Avalanche Summary

A very active period of spring avalanche activity started Friday and has continued through Wednesday. Wet/loose natural and controlled avalanches have been widespread with numerous sz 3, and isolated sz 4's. Many slidepaths failed down to ground once the avalanches reached Treeline elevations and lower. The number of avalanches has started to taper off, but large destructive avalanches are still possible.

Snowpack Summary

Warm temps have penetrated the snowpack creating an moist, isothermal snowpack treeline and below on all aspects and into the alpine on solar aspects. Buried crusts in the upper 50 cm are breaking down. Shallow snowpack features have loose, weak snow to ground.

20-40cm above the ground the Nov 17 basal weakness can still be found in many areas.

Weather Summary

As the high pressure weakens, freezing levels will start to drop and convective showers will develop, with rain/snow forecast for the weekend.

Tonight: Cloudy, Alpine Low 9°C, FZL 3500m, light ridgetop wind

Thurs: Mix of sun/cloud w. isolated showers, Alp High 15°C, FZL 3700m, light, gusting to mod E winds

Fri: Mix of sun/cloud, Alp high 12°C, FZL 3500m, light, gusting to mod E winds

Terrain and Travel Advice

  • Avoid the runout zones of avalanche paths. Very large avalanches have been running full path.
  • As surface loses cohesion due to melting, loose wet avalanches become common in steeper terrain.
  • If triggered loose wet avalanches may step down to deeper layers resulting in larger avalanches.

Problems

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.

Deep Persistent Slabs

Deep Persistent Slab avalanches are the release of a thick cohesive layer of hard snow (a slab), when the bond breaks between the slab and an underlying persistent weak layer deep in the snowpack. The most common persistent weak layers involved in deep, persistent slabs are depth hoar or facets surrounding a deeply buried crust. Deep Persistent Slabs are typically hard to trigger, are very destructive and dangerous due to the large mass of snow involved, and can persist for months once developed. They are often triggered from areas where the snow is shallow and weak, and are particularly difficult to forecast for and manage.