Typical size distributions for airborne particles are described and the sig
nificance of the ultrafine fraction highlighted. Size distributions may be
expressed in terms of either mass (volume), surface area or number, and the
interpretation of each is discussed together with appropriate measurement
methods. The sources of ultrafine particles in the atmosphere include both
primary emissions and secondary particles formed through homogeneous nuclea
tion processes within the atmosphere. Examples of measurements of atmospher
ic ultrafine particles are given, highlighting situations with high concent
rations of primary ultrafine particles and also situations where gas-to-par
ticle conversion through homogeneous nucleation gives rise to bursts of new
particle production. Finally, the relationship between particle mass and n
umber within the atmosphere at a polluted site is examined.