TetonSnowInfo

At the upper elevations, gusty winds continue to transport snow onto leeward terrain features and form small, pockets of slab avalanches. These slab avalanches could be human triggered on steep, avalanche-prone terrain and will likely have severe consequences in extreme terrain. The daily warming will increase the possibility to trigger these slabs and may cause small, wet loose avalanches on steep sunlit slopes. These hazards could impact skiers and snowboarders who venture onto hanging snowfields or into cliff areas and steep couloirs. At the mid and lower elevations, avalanches are unlikely but monitor the daily warming for changes in conditions.