ABSTRACT The edge row of dwarf apple trees was sprayed with an air sprayer; fluorescent dye was used to trace spray drift deposits. Tracer deposited on the ground was measured with plastic collectors and airborne spray was captured and measured with string, bottle, and high-volume, air-sampling filter collectors. Microclimatic variables including vertical heat flux were measured. Ground deposit decreased greatly beyond 120 m; about 0.03% of total material sprayed was deposited between 122 and 152 m downwind. Airborne spray between the ground and a 20 m level at 122 m downwind was estimated to be about 3.5%. Ground collectors and an unobstructed array of string collectors located 5.0 m from the sprayer captured about 75% of the total material sprayed.