Wind that started in late afternoon of 12/27 had transported significant amounts of new snow, creating fresh drifts in exposed terrain that were sensitive to the weight of a skier. In the Boulders, along exposed major ridge lines, these drifts were quite stiff (P) and up to 30cm thick.
Steady moderate north winds blowing above 9,000', increased to steady strong above 10,000' with occasional extreme gusts. Observed significant amounts of snow being transported in the Western Smokys throughout the afternoon.
Spotted a few small drifts that failed naturally in heavily loaded terrain. These drifts were sitting on either slick alpine surfaces or stacks of facets.
Problem | Location | Distribution | Sensitivity | Size | Comments |
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Wind Slab |
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Persistent Slab |
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Layer Depth/Date: 12/7 SH Comments: Faceting/breakdown of overlying slab is making it harder to trigger large, far-traveling collapses. However, numerous small collapses were experienced at lower elevations. In middle elevations this problem wasn't present where we traveled (likely a combination of poor environment for both SH generation and pre-burial preservation). With a significant load, I'd anticipate that this problem will rear its head again. |
Avoided steep terrain with recent wind slabs. Avoided avalanche terrain where 12/7 SH existed with a strong overlying slab.