Wet Slabs
- Alta montaña
- Límite del bosque
- Bajo el límite del bosque
- Probabilidad
- Likely
- Tamaño
- 1–2
After several warm days and cool nights, water appears to be reaching weak layers and crusts in the upper snowpack. Two avalanches were triggered yesterday afternoon, one remotely by a forecaster south of Teton Pass in a sunny, wind protected bowl and one triggered by a snowcat pushing snow onto a sun-baked slope at JHMR (see photo).
Recent avalanche activity prior to these two slides was limited to wet loose sluffs, a few of which were large and potentially dangerous. Those occurred primarily on the first warm day last week (Thursday and Friday) when sun heated up fresh snow. Since that time, every day seemed to be a replay of the previous one, with sunlit surfaces becoming wet 3-4" down but no reported wet sluffs or slabs. Recent snowpits are now showing water pooling on crusts at various depths beneath layers of dry snow. Assessing the exact location and depth of these crusts prior to skiing a slope isn't really feasible due to the spatial variability of the layers, but observing the warm temps, calm winds and slush on the surface is easy. Monitor the snow surface as the day heats up. Surface crusts formed overnight melt quickly in areas that experienced a light freeze and will send more water into the snowpack. Think twice if you are sinking in past your ankles and be mindful of potentially forceful, wet loose avalanches, even on less sunbaked slopes.
(3/19/2024) This avalanche was triggered by a snowcat pushing snow onto a ski slope yesterday afternoon.