Spray transects through an 11-m-tall pecan orchard with an air-blast orchard sprayer were replicated 10times over a wide range of atmospheric stability conditions. Drift was measured by collecting tracer (malathion) usingground plates (f), high volume air samplers (hv), and string (s) collectors distributed downwind in the adjacent field outto a maximum distance of 18 canopy heights (198 m). Atmospheric conditions were measured above the orchard canopywith fast-response, three-dimensional wind, temperature, and humidity sensors. Atmospheric stability, characterized bythe surface layer stability parameter ( ), was the primary factor affecting drift amounts measured on and above theadjacent field. On average, the total amount of drift caught by the samplers in very stable conditions was 5.9, 3.6, and 2.1times the amount of drift in unstable conditions for the plates, the hvs, and the strings, respectively. The transition fromone condition to the other took place over a very small stability range where the air was dynamically stable (0.0 < <0.3). In this range, very small changes in atmospheric conditions resulted in very large changes in the atmospheresaerosol transport characteristics. The effect of stability on the amount of drift collected in the adjacent field is describedby a symmetric hyperbolic tangent function over the entire range of stability encountered.