Bollettino valanghe

Central Sierra Nevada

Sierra Avalanche Center
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Pericolo valanghe

Sun
Alta quota
2 · Moderato
Limite del bosco
2 · Moderato
Sotto il limite
2 · Moderato
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Non aggiornato — questo bollettino è scaduto 3 years ago. Stai vedendo condizioni passate, non il bollettino in corso.

In sintesi

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.

Problemi valanghivi

  • Persistent Slabs

    • Alta quota
    • Limite del bosco
    • Sotto il limite del bosco
    Probabilità
    Possible
    Dimensione
    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.

Regioni coperte