Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind slabs from the recent storm may have formed over weak snow grains in alpine areas on northerly aspects. And while much of the East Central zone didn't receive enough snow for this to be a significant problem. Areas near the crest, particularly in the Salmon la Sac drainage, may have seen snow totals closer to those of Snoqualmie Pass. The Salmon la Sac area may even continue to see snow accumulations into the morning hours of Wednesday. If you find more than 8 inches of fresh snow over the Early March Crust, be especially cautious of traveling on northerly aspects near ridgelines in steep terrain above 5500ft as you may be able to trigger an avalanche large enough to bury or kill you. There is uncertainty and variability with the distribution of these weak faceted snow grains. Similar slopes may react differently, so enter new terrain slowly and make observations before committing to complex or steep terrain.Significantly less snow fell in areas further east in the zone. However, if you travel to alpine areas, look for signs of instability in wind affected terrain. Shooting cracks, feeling the snowpack collapse beneath you, or recent avalanche activity are all bullseye signs of an unstable slope. You can also dig down quickly to observe if the snow slides easily off the crust and look for weak snow just above the crust. If the snow easily slides on the crust, you find it weak snow, or see other signs of instability stick to conservative terrain with lower angle slopes.
Example of wind slab in alpine terrain.