Spectral UV irradiance on vertical surfaces: A case study

The UV spectral irradiance on horizontal and vertically oriented surfaces w as measured throughout a cloudless day (18 July 1995) at Izana station, Ten erife, using a Bentham DTM300 spectroradiometer scanning from 290 to 500 nm in steps of 5 nm, Results show that irradiance measured on a horizontal su rface is not proportional to irradiance on a vertical surface. The relation between the two depends upon orientation of the vertical surface, zenith a ngle and wavelength. At short UVB wavelengths surfaces directed toward the solar azimuth received their maximum irradiances much closer to solar noon than the maxima for longer wavelengths. Some vertical surfaces also receive d significantly more irradiance than the horizontal surface at long wavelen gths during all but the central hours of the day, while at short wavelength s all vertical irradiances were less than the horizontal except for the mea surements at the extreme ends of the day. Erythemally effective radiation f ollowed the diurnal pattern of irradiations for short UVB wavelengths.