Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Likely
- Size
- 1–2.5
Yesterday afternoon and into this morning we received around 5.4 inches of new snow, with 0.46 inches of SWE, on the summit of Mount Washington. Consistently strong winds from the west and northwest have moved snow from the fetch of the upper snowfields down lower into steep gullies and ravines. Drifted slabs of wind transported snow have formed that could be 1 to 2 feet thick in the upper elevation starting zones. Some of these slabs could be reactive or even touchy in their sensitivity to human triggering.
It is possible to see evidence of natural avalanches in and below steep ski terrain this morning. It is even more likely that lingering slabs of consolidated wind-transported snow still reside above you in the starting zones and the tract of popular ski runs. Older drifted slabs, from earlier in the week, may become reactive with new snow loading them to the threshold of failure. Step down avalanches are a primary concern when we get repeated storms in succession and no time for proper settlement between them.