An investigation has been carried out into the possibility of using polarization methods to characterize clouds of irregular particles. Measurements were made at scattering angles between approximately 115 • and 135 • , where it was expected that polarization effects would have maximum variation with shape. It was found that the angular variation of any polarization property was similar for most particles. Further, as a consequence of reciprocity, the useful parameters were limited to the scattered intensities for two incident polarization states and one cross-polarized intensity. The only useful correlation appeared to be between cross-polarization and the 'roundness' of the particles, although different correlations are observed between particles which are inherently isotropic and those which are anisotropic. The main conclusion of the study is that polarization can be used to measure the average roundness of particles in a cloud and has the potential to discriminate between crystals of different structure.