To answer the question the title poses: yes! On this chilly, moist morning in downtown Wichita, the fuzzy base of the stratus deck engulfed the tops of the buildings, but became fog at ground level, some indeterminate distance northward. Drizzle also fell at this time and location, which is common in foggy boundary layers under strong low-level warm-advection regimes.
Wichita KS (10 Feb 19) Looking NNE
37.6829, -97.3417