Avalanche forecast

Central Sierra Nevada

Sierra Avalanche Center
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Avalanche danger

Fri
Alpine
2 · Moderate
Treeline
2 · Moderate
Below
2 · Moderate
Out of date — this forecast expired 4 years ago. You’re viewing past conditions, not the current bulletin.

Highlights

The likelihood of triggering an avalanche has decreased somewhat. Obvious signs of instability are presenting less frequently making a truly accurate slope scale stability assessment more challenging. If you trigger an avalanche today, it will be big.

Avalanche problems

  • Persistent Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    2–3

    We've now made it through three days with no reported avalanches. Snowpack data is still coming in daily pointing out that the instability is still there. Now we are at the most challenging part of this avalanche cycle. Collapses and whumpfing have become less common and snowpit test results are more variable or harder to trigger. It is not uncommon for a persistent slab avalanche to occur after days of no avalanches, such as a day like today. If a slope is going to avalanche, it's going to go big.

    The Dec 1 persistent weak layer remains weakest on NW-N-NE aspects above about 8,000'. It is buried 1.5 to 4 feet deep near the bottom of the snowpack. Avalanches that have occurred on this weak layer have had a minimum size of D2 and wide propagation. Expect the same for any avalanches that are triggered today.

    If you choose to enter avalanche terrain today it is a high consequence environment. Large, wide propagating avalanches are difficult to survive. Anticipate that any avalanches triggered will be bigger, wider, and run longer downslope than expected. Previous tracks on a slope are not an indication of stability for this type of avalanche problem. I won't be surprised to hear about an avalanche that takes out previous tracks. Luck and skill may have similar outcomes in the backcountry, but they are not the same thing.

    (12/7/2022)

    One of two wide propagating natural avalanches on this slope. Likely occurred on Dec 3 or 4. N aspect terrain around 7,700'. Deer Creek drainage near Mt. Watson, CA.

  • Wind Slabs

    • Alpine
    • Treeline
    • Below treeline
    Likelihood
    Possible
    Size
    1–1.5

    There is plenty of low density snow on the ground near ridgetops available for wind transport. Increasing ridgetop winds today will create areas of blowing and drifting snow. New wind slabs are expected to form near treeline and above treeline on NW-N-NE-E-SE aspects. Anywhere you see blowing snow, expect to find a fresh wind slab on the downwind side of the ridgetop. Identify and move cautiously around cornice areas and other slopes with obvious wind loading.

Avalanche Discussion

  • Spatial variability is increasing for signs of instability on the faceted Dec 1 PWL. Some areas still show significant indications of instability while others do not. It would be easy to incorrectly assess slope scale stability at this time.
  • Much of the surface hoar that exists will be knocked down or destroyed today by increasing winds. If you are out today and the winds have been blowing for a while, keep an eye out for any upright, intact surface hoar. If you see any, please use the submit observations link to send us a photo and location info.

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