Wind Slabs
- Alpine
- Treeline
- Below treeline
- Likelihood
- Possible
- Size
- 1.5–3
Strong North winds began to affect our area on the 29th redepositing significant amounts of dry snow and building deep wind slabs. Wind speed peaked on the night of the 30th with gusts in the mid 60's on Thompson Pass. During this time numerous natural avalanches occurred up to size 3. Winds are on a slow decline but are expected to continue to be at least moderate through wind channeled terrain like Thompson Pass and high elevation ridges.
Expect to find an array of wind-damaged snow out there today with wind slabs on lee aspects 1-3+ feet in depth. These wind slabs are now a few days old and are becoming harder with age. This increase in strength will make slabs stubborn- unreactive to triggers but if one were to fail it would have the potential for wide propagations, and could fail behind you once you have already traveled out onto the slab. The likelihood of human-triggered avalanches is decreasing, but still should be considered as consequences would be high due to the knife hard snow that would be involved.
Wind slabs will have a hollow-drum-like feel and can have a smooth pillowed look or a rippled texture. These will exist on the lee side of terrain features, cross loaded slopes and just below high elevation ridges. Signs of instability are not likely to exist, but if they are encountered it is a a bullseye sign of instability.
In areas where the snow is protected from the wind, good stability and snow structure have been observed as recently as 1/31.
(1/30/2025)
Remote triggered Hard slab. Comstock lowers.
Photo: Gareth Brown