From a data archive of spectral energy distribution of global and diffuse solar irradiances measured in Athens during a field experiment, the influence of atmospheric turbidity caused by urban aerosol on spectral composition of visible radiation and transparency of urban atmosphere has been determined for cloudless conditions. The effect of urban aerosol is significant in the PAR part of solar spectrum, where attenuation of global PAR irradiance surpasses 18% on very polluted atmospheric conditions. The increase in diffuse PAR irradiance caused by urban aerosol ranges in the interval 7%–51%. The ratio of global PAR to total global irradiance was found to depend slightly on air pollution whereas ratio's dependencies on site elevation were not identified clearly. Nevertheless, this ratio was found to be in good agreement with those reported in the literature. The ratio of diffuse-to-global PAR irradiance was found to depend on both, air mass and turbidity. For very turbid atmosphere and large air masses the 40% of PAR irradiance results from diffuse radiation. Finally, some biological implications of the results are briefly discussed.