Boletín de aludes

Whitefish Range

Flathead Avalanche Center
Ver en el mapa

Peligro de aludes

Wed
Alta montaña
1 · Débil
Límite del bosque
1 · Débil
Bajo el límite
1 · Débil
Open full map
Desactualizado: este boletín caducó 3 years ago. Estás viendo condiciones pasadas, no el boletín vigente.

Lo esencial

Riders found generally stable avalanche conditions this past weekend. Small slabs of drifted snow may remain sensitive to the weight of a rider due to the weak snow they rest on. Stear around dune-shaped drifts while seeking out snow sheltered from the wind. 

Problemas de aludes

  • Wind Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Unlikely
    Tamaño
    1–1.5

    Look for and steer around signs of obvious drifting near ridgelines and on cross-loaded gullies further downslope. Pillowy-looking surfaces or surfaces with a textured appearance are visual clues of a Wind Slab. Slabs of drifted snow should be harmless in size by themselves, though they could be consequential if caught above a cliff or stand of trees. Slopes sheltered from the wind will hold safer and better riding conditions. 

Avalanche Discussion

On Friday and Saturday, a winter storm brought 8 to 12 inches of snow to the Flathead Range/Glacier National Park forecast zone. The Swan Range and Whitefish Range received only 2 to 4 inches of snow. With this snowfall came moderate wind speeds, which are ripe speeds for drifting snow into thicker slabs. Since then, we have received numerous reports of natural avalanches, human-triggered avalanches, and signs of unstable snow. Here are a few noteworthy observations from each forecast zone (Flathead, Glacier National Park, Whitefish, Swan). 

On shaded aspects, storm snow fell on a weak layer of facets. This sugary snow is the culprit for recent avalanche activity. Unfortunately, this weak layer may be slow to heal, which is one of the reasons we transitioned to a Persistent Slab avalanche problem in the Flathead Range. Another reason is that avalanches are breaking in surprising ways by wrapping around terrain features and being remotely triggered. This requires a wider margin for error by putting more space between you and the steep slopes that harbor this structure. This structure is primarily found on northerly aspects above roughly 6000 feet.

On south and west-facing slopes, recent snow fell on a melt-freeze crust. Observations suggest that it is less likely to trigger a slab avalanche on those aspects. However, if you plan to travel on solar aspects today, keep an eye on cloud cover and surface warming. If the sun sticks its face out longer than expected, plan to see some rollerballs and small wet loose activity out of steep rocky areas. This will be more common in the Flathead Range where more snow fell. A sun crust may already exist on some solar aspects.

Continue to steer around signs of wind-drifted snow in the Swan and Whitefish Ranges. Slabs of drifted snow sit on weak snow that will be slow to heal. Pockets of drifted snow should be easy to identify by their textured appearance. 

FAC will issue daily forecasts through Easter Sunday, April 9. Following this, we will give snowpack updates several times a week through April if conditions dictate. 

Regiones cubiertas