We assume the initial moisture content is set by an RH in the mouth of 99.5 % and a temperature of 308 K (35 o C), 139 m in a 50% RH environment over 3.6 s before the droplet sediments to the ground, travelling a horizontal distance of 0.97 m from source. Indeed, the droplet is not equilibrated at deposition requiring a full 30 s to reach within 5 % of its final equilibrated size (42.0 m). In other words, most of the moisture loss occurs after the droplet has deposited onto the ground. By contrast, a 60 m diameter droplet evaporating in a 50% RH environment equilibrates to a size of 17.0 m within 7.2 s, completing equilibration well within the 70 s it takes to sediment to the ground. This droplet travels a horizontal distance of 2.9 m from the source. Droplets with an initial diameter < 60 m do not sediment at all within the horizontal distance of 4 m from the source and fully equilibrate with the ambient RH in <7 s. These droplets shrink to around 29% of their initial diameter.