Wind drifts - both new and old - remain the primary concern in the Provo mountains. The old ones are becoming increasingly stubborn, but they are not dormant. They are more prominent in the upper elevations but also noted to the lee of exposed mid-elevation ridgelines. They'll be more prominently found on steep north to east to south facing terrain; even cross loaded on some southwest facing slopes. The new ones will be shallow but more sensitive in the upper elevations and exposed ridgelines of the mid-elevations.