New experiments have succeeded in measuring actual rates of nucleation
and are revealing the shortcomings of classical nucleation theory, wh
ich assumes that the molecular-scale regions of the new phase may be t
reated using bulk thermodynamics and planar surface free energies. In
response to these developments, new theories have been developed that
incorporate information about molecular interactions in a more realist
ic fashion. This article reviews recent experimental and theoretical a
dvances in the study of nucleation of liquids from the vapor and of cr
ystals from the melt, with particular emphasis on phenomena that relat
e to particle formation in the atmosphere.