Thousands of basidiomycete fungal species rely on mushroom spores to spread across landscapes. It has long been thought that spores depend on favorable winds for dispersal-that active control of spore dispersal by the parent fungus is limited to an impulse delivered to the spores to carry them clear of the gill surface. Here we show that evaporative cooling of the air surrounding the pileus creates convective airflows capable of carrying spores at speeds of centimeters per second. Convective cells can transport spores from gaps that may be only 1 cm high and lift spores 10 cm or more into the air. This work reveals how mushrooms tolerate and even benefit from crowding and explains their high water needs.ooted in a host organism or patch of habitat such as a dead log, tens of thousands of species of filamentous fungi rely on spores shed from mushrooms and passively carried by the wind to disperse to new hosts or habitat patches. A single basidiomycete mushroom is capable of releasing over 1 billion spores per day (1), but it is thought that the probability of any single spore establishing a new individual is very small (2, 3). Nevertheless in the sister phylum of the basidiomycete fungi, the Ascomycota, fungi face similarly low likelihoods of dispersing successfully, but spore ejection apparatuses are highly optimized to maximize spore range (4-6), suggestive of strong selection for adaptations that increase the potential for spore dispersal.Spores disperse from basidiomycete mushrooms in two phases (7): a powered phase, in which an initial impulse delivered to the spore by a surface tension catapult carries it clear of the gill or pore surface, followed by a passive phase in which the spore drops below the pileus and is carried away by whatever winds are present in the surrounding environment. The powered phase requires feats of engineering both in the mechanism of ejection (8-10) and in the spacing and orientation of the gills or pores (11,12). However, spore size is the only attribute whose influence on the passive phase of dispersal has been studied (13). Spores are typically less than 10 μm in size, so can be borne aloft by an upward wind of only 1 cm/s (11). Buller claimed that such wind speeds are usually attained beneath fruiting bodies in nature (11): Indeed, peak upward wind velocities under grass canopies are of order 0