Boletín de aludes

Central Sierra Nevada

Sierra Avalanche Center
Ver en el mapa

Peligro de aludes

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

Lo esencial

A weak and problematic snowpack exists in portions of the forecast area.  Evidence of the current snowpack instability is not obvious. Thoroughly assess the snowpack before committing to avalanche terrain on shaded slopes. Opt for lower angle, non-avalanche terrain if any indications of instability are present.

Problemas de aludes

  • Persistent Slabs

    • Alta montaña
    • Límite del bosque
    • Bajo el límite del bosque
    Probabilidad
    Possible
    Tamaño
    2

    A cohesive slab over layers of faceted (sugary) snow that are found mostly within the lower half of the snowpack is the problem. The snowpack structure changes with elevation and location, with variability in layer weakness from one spot to another around the forecast area. Currently, the areas of greatest concern are found on NW-N-NE aspects above about 8,000' to 8,300'. Snowpit tests continue to show weakness and unstable results on various well developed weak layers.  Any avalanche involvement with this persistent slab problem could have high consequences from trauma due to our rocky, shallow snowpack.

    Unless you are specifically looking, signs of instability associated with the current avalanche problem are not obvious. Utilizing non-avalanche terrain under 30 degrees in steepness without steeper connected terrain above is a good strategy to minimize exposure and manage the increased physical consequences of becoming caught in an avalanche at this time.

Avalanche Discussion

A weak faceted (sugary) snowpack exists on most NW-N-NE aspects starting above about 7,400'.  Near and below about 8,500', faceted snow exists around and in between rain crusts. Gaining elevation above 8,500', rain crusts gradually disappear or decompose and the lower half of the snowpack becomes nearly all weak faceted snow. Generally speaking, the higher up you go on wind protected NW-N-NE aspects, the weaker the snowpack. These weak layers are well developed, with depth hoar found at the base of the snowpack in many areas. Low sun angles that leave northerly aspect slopes in the shade all day combined with long nights have kept weakness in our shallow snowpack ongoing.

There is still the potential to hit many obstacles (rocks, logs, open water, bushes, etc.) that are barely covered (or not) by the shallow snowpack. This is especially true in areas below 7,500' and in very rocky areas up to at least 8,000'. Anticipate encountering a different snowpack structure and a different set of travel conditions if you are moving from one place to another around the forecast area.

Regiones cubiertas