OBSERVED INFLUENCE OF CLOUDS ON ULTRAVIOLET-B RADIATION

Brewer Spectrophotometer was utilized to make ground-based measurement s of solar ultraviolet (WE) radiation received at Black Mountain, NC ( 35.66 degrees N) in order to quantify the reduction of UV-B due to clo ud cover. Observations were made over the interval February-July 1995 with continuous coverage except for a three-week period in May. A wide -angle lens video camera at the site was used for the assessment of cl oud conditions at the time of each scan. integrated UV-B (290-320 nm) values were evaluated and a regression through the values for clear co nditions was produced for the range of zenith angles from 25 degrees - 70 degrees. This regression effectively represents an average effect of the ambient aerosols and attenuating gases and was used to normaliz e the UV-B values measured under different cloud cover an estimate of the reduction in irradiance due to a given cloud amount as a function of solar zenith angle. For a solar zenith angle of 50 degrees, average UV-B transmission was observed to be 30% for overcast skies, 6156 for 8-9 tenths cloud cover, 74% for 6-7 tenths cover, and 79% for the sca ns during 4-5 tenths cover. A number of fractional cloud cover cases w ere observed where cloud reflections resulted in measured surface irra diances exceeding the expected clear sky values by as much as 11 perce nt.