Abstract: No Abstract Available

Abstract: An explanation is offered for the similarities observed experimentally among size distributions of natural aerosols measured at different places and times. This explanation is based on a similarity transformation of the ...

Abstract: An equation is derived for the time rate of change of the size spectrum function of the stratospheric aerosol. Based on the assumption of local equilibrium between the effects of coagulation and sedimentation, a form is ...

Abstract: Distribution data obtained by sampling the Baltimore aerosol with a cascade impactor are reported for the range between 0.4 and 20 microns radius. Data for the range between 70 Å and 0.1 microns in radius were obtained in ...

Abstract: Previous experimental measurements of particle size spectra of the atmospheric aerosol are reviewed. A four-stage impactor was used to sample the Baltimore aerosol in the size range above 0.4 microns in radius. Particle ...