Wind Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Possible
- Tamaño
- 1–2
Over the past week, this zone has received a constant trickle of snowfall accompanied by light to moderate winds, and this pattern continued yesterday and overnight. The low-density nature of the new snow has made it easily transported by even light breezes. Wind slabs may be found near ridgelines or mid-slope in exposed terrain. The lower elevations of the Banner Summit zone mean that wind loading can be more subtle—assume that all open or sparsely treed, upper elevation slopes have experienced at least some amount of wind loading over the past week.
ADDITIONAL DISCUSSION:A number of weak layers—both prominent and subtle—exist in the top 3' or so of the snowpack. None of these seem particularly reactive but have still produced a few small to medium-sized avalanches in the past week. Nearly constant loading from light snowfall and wind over the past week are not giving these weak layers any relief. One of these layers is the likely culprit behind the snowmobile-triggered avalanches near Cape Horn Summit on Tuesday (photo to right/above), and a skier yesterday triggered a slide in very steep terrain. And we can't forget the early-season weak layer near the base of the snowpack. You would have to be unlucky to trigger a slide this deep, but this layer has kept us out of the terrain where it is most likely to exist—namely very steep, rocky, and wind-affected terrain at upper elevations.
You can greatly reduce your chances of triggering an avalanche of any variety by avoiding "prime-time" slopes over about 35 degrees, especially in wind-exposed upper elevation terrain.
(2/16/2021) A snowmobiler triggered this avalanche from the bottom of the slope on Tuesday afternoon near Cape Horn Summit.