Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1–2
Wind slabs were reported as easily triggered on Friday near treeline on slopes where wind blown snow was accumulating. Often times, wind slabs are most sensitive to triggering when they are newly formed. With wind speeds expected to back off on Saturday, we may see light amounts of blowing snow, but the bulk of the wind slab formation occured on Friday. Wind slabs need more time to bond and heal. It is too soon to take these off the list and wind slabs will still be possilbe to trigger on Saturday.
Remember, wind slabs can be many times deeper than the amount of snow that fell during the storm. Montior the depth of wind drifted snow as you move through lee terrain below ridge tops. As you observe increased depth of wind loaded snow, expect resulting avalanches to become larger. Ease into steeper terrain. Look for cornices at ridgetops and rough, wavy, or chalky surface texture on lee slopes to indicate where wind slabs have formed. If you encounter cracking in wind drifted snow, or observe recent avalanches, that is a good indication to stay off of slopes steeper than 30 degrees.