Central Sierra Nevada

Lawinenprobleme

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  Wind Slabs

  N

  NE

  E

  SE

  S

  SW

  W

  NW

  • Hochgebirge
  • Waldgrenze
  • Unterhalb der Waldgrenze

  Wahrscheinlichkeit

  Likely

  Größe

  1

  New snow and gale force SW winds over the past 24 hours increased the existing wind slab problem. Unstable wind slabs were reported yesterday from numerous areas. A small skier triggered wind slab avalanche was intentionally triggered yesterday near Yuba Pass near treeline on a NE aspect at around 7,700'. In many areas, especially near treeline, slabs of wind drifted snow were deposited on top of weak faceted (sugary) snow. These wind slabs are expected to continue to be reactive today. Problematic wind slabs are widespread near treeline and above treeline on NW-N-NE-E aspects across the forecast area.

  Any slopes near ridgetops where blowing and drifting snow have deposited are suspect. Any slopes with newly formed cornices or drifted pillows of snow along the upper portion of the slope are likely to hold unstable wind slabs. Snow surface cracking is a sign of unstable snow in the immediate area. Use low angle or wind protected terrain to avoid the areas where wind drifted snow is depositing as a wind slab. Take care not to venture onto slopes with a persistent slab problem while trying to avoid the wind slab problem.

   Small wind slab avalanche intentionally triggered yesterday near Yuba Pass, CA.

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  Deep Persistent Slabs

  N

  NE

  E

  SE

  S

  SW

  W

  NW

  • Hochgebirge
  • Waldgrenze
  • Unterhalb der Waldgrenze

  Wahrscheinlichkeit

  Likely

  Größe

  2

  Evidence of the expected persistent slab avalanche problem began to show yesterday afternoon. The long dry spell from Nov 18 to Dec 11 caused the existing snowpack to weaken and turn sugary from the faceting process. This weak snow is widespread below treeline and near treeline on W-NW-N-NE-E aspects. It has been noted in isolated areas above treeline as well. The snowfall from the past 24 hours is expected to have brought this weak snow very close to the point of failure. The added weight of a person may be all that is needed to trigger an avalanche. Persistent slab avalanches will break in the snowpack below the old/new snow interface and could have wide propagation, wrapping around corners and other terrain features that often confine wind slabs and storm slabs. Persistent slab avalanches can be triggered in low angle terrain from a distance to the side, above, or from below (remote triggering). In some cases with this type of avalanche problem, an avalanche may occur on a slope that already has tracks on it.

  Staying on wind protected slopes in the trees is not a tactic for avoiding persistent slabs. It is a tactic for avoiding wind slabs. You have to route plan to manage both today. The situation is now complex with travel in avalanche terrain difficult to manage. The easy answer is to pull back into low angle, conservative terrain that is less than 30 degrees in slope angle and without steeper slopes adjacent or above.

   Shooting crack failing on old faceted snow below 8 inches of new snow load in the Mt Rose zone, NV.