An experiment was conducted over a B-month period in Research Triangle
Park, North Carolina, to investigate the effects of clouds and haze o
n ultraviolet (UV) radiation. Data were collected using a Yankee Envir
onmental Systems UVB-1 pyranometer, an Eppley Laboratory Precision Spe
ctral Pyranometer, and a SCI-TEC Brewer spectrophotometer. Hourly repo
rts of total cloud cover and surface observations of air temperature,
dew point temperature, barometric pressure, and visibility from the Na
tional Weather Service located at the nearby Raleigh-Durham Internatio
nal Airport were also used in this study. An empirical relationship ha
s been formulated for UV-B attenuation as a function of total solar tr
ansmissivity and cloud cover. Cumulus-type clouds were found to attenu
ate up to 99% of the incoming UV-B radiation during overcast condition
s. However, these same clouds were found to produce localized increase
s of UV-B radiation of up to 27% over timescales less than 1 hour unde
r partly cloudy skies when the direct solar beam was unobstructed. Sum
mer haze was found to attenuate UV-B radiation in the range of 5% to 2
3% when compared to a clear day in the autumn. In general, total radia
tion was attenuated more than UV-B radiation under cloudy conditions.